<p>The Justus Ramsey Stone House is the oldest known house still standing in Saint Paul in the USA state of Minnesota. The house, located at 252 West 7th Street is listed on the National Register of Historic Places. The home is an example of a Saint Paul residence of a settler of some financial means.</p><br>
<h2>Ramsey</h2><br>
<p>Justus Cornelius Ramsey was born in Hummelstown, Dauphin County, Pennsylvania and learned the printer&#39;s trade. He was first employed as a surveyor for the Pennsylvania Railroad, then came to Saint Paul in 1849 where he engaged in the grocery business and in real estate. He was the younger brother of the first governor of Minnesota Territory, Alexander Ramsey. In 1850, he was elected to the Minnesota Territorial Legislature and served for three terms; he also served in other governmental posts, including carrying the treaty payment to the Dakota when the Dakota War of 1862 erupted.</p><br>
<h2>The building</h2><br>
<p>The 35-acre (14 ha) parcel including 252 West 7th Street was purchased by Henry Hastings Sibley, Henry M. Rice, and Justice Ramsey for $60.00 in 1849. The land was subdivided in 1850, and Justus Ramsey kept the title to the lot where this two-room house was built; it is believed that he initially lived in the home. It was constructed with 2-foot-thick light gray quarry-faced limestone walls, ashlar-coursed with lime mortar. In 1859, Ramsey lost or sold the home, after which it served as a barber shop and a residence.</p><br>
<p>Ramsey committed suicide in 1881, leaving behind a fortune of $200,000.</p><br>
<p>Valley Grove refers to two religious buildings situated near the community of Nerstrand in rural Rice County, Minnesota. The Valley Grove church buildings are located south of Northfield, Minnesota near Big Woods State Park at 9999 155th St E, part of Valley Grove Road .</p><br>
<p>The Lutheran congregation discontinued use of the location in 1973. The Greek Revival churches were listed on the National Register of Historic Places during 1982. Today, both buildings are maintained by the Valley Grove Preservation Society. Valley Grove is the site of an annual country social, weddings and concerts including its Christmas Eve celebration.</p><br>
<p>The churches were built on a grassy knoll by Norwegian immigrants who first came to eastern Rice County beginning around 1850-1860. The older stone building was built in 1862 and is currently undergoing renovation; the Valley Grove Preservation Society obtained a fifty-year lease on the building from the Valley Grove Grace Cemetery Association in 2007. In subsequent years, the church has received a new steeple roof, finials, exterior repairs and painting. This project has been financed in part with funds provided by the State of Minnesota through the Minnesota Historical Society from the Arts & Cultural Heritage Fund.</p><br>
<p>The other newer church was built just a few steps away in 1894 and features white clapboard siding. The newer building has already been renovated and is utilized principally for local ceremonies and celebrations. In the adjacent cemetery, many of the headstones were worded in the Norwegian language. The graveyard contains the Veblen family plot, whose members lived at the nearby Thorstein Veblen Farmstead.</p><br>
<h2>Bernt Julius Muus</h2><br>
<p>In 1859, the Norwegian Lutheran pastor, Bernt Julius Muus baptized 52 children on the site. Muus was born in Snåsa, Trøndelag, Norway and completed his theological training in 1854 before emigrating in 1859. In 1875, he helped found St. Olaf College. Although his achievements were great, he was often brusque and uncompromising; as a result he was later expelled from the church for his stubborn nonconformity.</p><br>
<p>Giant&#39;s Hole is a well-known cave near Castleton in Derbyshire, consisting mostly of large passages. It is a stream-way cave, and part of the Karst topography of the area.</p><br>
<p>There is a complex system connecting the cave to Oxlow Cavern and Maskhill Mine to the south. The Entrance Series is easily accessible making it a favourite with novices and groups. The stream that flows into the entrance can be followed through the cave, bypassing three sumps, to the East Canal, Giants Holes terminal sump.</p><br>
<p>There are several major tributary passages and a high-level fossil series that provides an alternative route through the cave and makes up part of the classic "round trip". East Canal has been dived to a depth of 24 m in drought (but water levels are normally much higher). The connection to Oxlow Cavern is a serious undertaking and many cavers have underestimated the difficulty of the passage.</p><br>
<p>Since 2002 the Derbyshire Cave Rescue Organisation has attended 11 callouts to Giant&#39;s Hole, one of which resulted in a fatality.</p><br>
<p>Lewis Smith Lake is a reservoir in north Alabama. Located on the Sipsey Fork of the Black Warrior River, the lake covers over 21,000 acre in Cullman, Walker, and Winston counties. The maximum depth at the dam is 264 feet. The three-fingered lake has over 500 mi of shoreline, and at full pool has a level of 510 ft.</p><br>
<p>The lake was created by Alabama Power with the construction of the Lewis Smith Dam. One of the largest earthen dams in the eastern United States, it stretches 2,200 ft in length and reaches a maximum height of 300 ft. Construction began on November 25, 1957, and the dam entered service on September 5, 1961. The name honors Lewis Martin Smith, president of Alabama Power from 1952 to 1957.</p><br>
<p>Nearby towns include Bremen, Crane Hill and Dodge City in Cullman County; Curry and Jasper in Walker County; and Addison, Arley, Houston, and Double Springs in Winston County.</p><br>
<p>The most popular tourist attraction on Smith lake is the Indian head cliff jump. Its 70 feet ( 21m ) and is located on the south shoreline of Smith lake. Its considered the most dangerous cliff jump located on Smith lake. There have already been two deaths reported where the victims just didn&#39;t surface. The bodies were later found.</p><br>
<p>Manilla River, a perennial stream that is part of the Namoi catchment within the Murray–Darling basin, is located in the Northern Tablelands district of New South Wales, Australia.</p><br>
<p>The stream (called a river) rises south–west of Barraba on the northern slopes of the Baldwins Range and drains a portion of the hill country on the western side of the New England highlands and the southern slopes of the Nandewar Range; flowing generally north and east and to the town of Barraba. During its course, the stream is joined by five minor tributaries, and flows in a southerly direction towards its confluence with the Namoi River at the town of Manilla; dropping 496 m over its length of 138 km.</p><br>
<p>The name of the river is derived from the Australian Aboriginal words of manilla, maneela, or muneela meaning "winding river" or "round about".</p><br>
<p>Approximately 10 km north of Manilla, Split Rock Reservoir, on the Manilla River, provides one of the main water storages for flood control and irrigation in the Namoi River basin.</p><br>
<p>The Horton River, a perennial stream of the Barwon catchment within the Murray-Darling basin, is located in the Northern Tablelands and North West Slopes districts of New South Wales, Australia.</p><br>
<h2>Course and features</h2><br>
<p>The river rises on the northern slopes of the Nandewar Range, below Mount Kaputar, and flows generally southeast and north, joined by six tributaries before reaching its confluence with the Gwydir River, north west of Bingara; descending 1,060 m over its 134 km course.</p><br>
<p>The valley of the Horton River is used for grazing and some cropping. It is a sparsely populated area with no significant towns. There is a small village called Upper Horton. The valley is traversed by the Narrabri-Bingara Road. Other nearby towns, outside the valley, are Barraba, Bingara, and Narrabri.</p><br>
<p>The Horton River is a source of floodwater for the Gwydir River and Mehi River and can flood the town Moree.</p><br>
<p>Cockburn River, a perennial river that is part of the Namoi catchment within the Murray–Darling basin, is located in the Northern Tablelands district of New South Wales, Australia.</p><br>
<p>The river rises in the west slopes of Moonbi Range, near Limbri and then flows generally west south west, joined by four minor tributaries, towards its confluence with the Peel River at Nemingha; dropping 109 m over its course of 33 km.</p><br>
<p>The river was first encountered by European explorers on 4 September 1818 during an expedition led by the Surveyor-General of New South Wales, John Oxley, who named the river in honour of Admiral Sir George Cockburn.</p><br>
<p>From upstream to downstream, the Cockburn River flows through or near the localities of Limbri, Moonbi, Kootingal, Tintinhull and Nemingha. A section of the Main North railway line runs along the valley of the Cockburn River.</p><br>
<p>The Cockburn River is also one of the fastest flowing rivers in the southern hemisphere. It is home to fish species including catfish, yellow belly, and European carp; the last have decimated the native fish stocks to the point that they are getting harder to find. There are small areas of irrigated cropping along the banks of the river and the surrounding hills are mostly used for grazing.</p><br>
<p>Gauss Peninsula  is a peninsula in eastern Greenland. Administratively this peninsula is part of the Northeast Greenland National Park zone.</p><br>
<h2>Geography</h2><br>
<p>The Gauss Peninsula is located between the Muskox Fjord (Moskusokse Fjord) and Kaiser Franz Joseph Fjord with the Nordfjord at its western end and the Foster Bay of the Greenland Sea shore on its southeastern side.</p><br>
<p>The peninsula is mountainous, with the Hjelm Range (Hjelmbjergene) located on the southern coast and the Giesecke Range (Giesecke Bjerge) located in the eastern part of the peninsula. Hold with Hope peninsula is located further to the east, beyond the Badland Valley (Badlanddal).</p><br>
<h2>History</h2><br>
<p>The second German North Polar Expedition 1869–70 originally gave the name Cap Gauss to a point on the south side of this peninsula, but A.G. Nathorst’s 1899 expedition was unable to determine the position because of the rounding of the coast and applied the name Gauss Halfö to the peninsula as a whole. It is named after German mathematician Carl Friedrich Gauss.</p><br>
<p>Kaiser Franz Joseph Fjord  is a major fjord system in the NE Greenland National Park area, East Greenland.</p><br>
<h2>Geography</h2><br>
<p>The Kaiser Franz Joseph Fjord has its mouth in the Foster Bay of the Greenland Sea, between Cape Mackenzie at the eastern end of Geographical Society Island and Cape Franklin, the southern end of the mainland&#39;s Gauss Peninsula; Bantekoe Island lies in the bay off its mouth. It extends westwards for about 100 km, then at Eleonore Bay in an NNE/SSW direction for about 32 km, bending again westwards at Cape Mohn, the western end of Ymer Island, branching again with the Isfjord extending northwestwards for over 60 km.</p><br>
<p>Two tributary fjords, the wide Nordfjord —with the large Waltershausen Glacier at its head—and the narrower Geologfjord —with the Nunatak Glacier, branch from the northern side of the fjord, about 70 km from the entrance. The Devil&#39;s Castle (Teufelsschloss) is a prominent mountain of reddish rock with a lighter stripe extending diagonally across its face that stands close to the southern side of Cape Petersens, the NW extremity of Ymer Island.</p><br>
<p>The fjord is bounded by the Suess Land Peninsula and Ymer Island to the South, and by Frænkel Land, Andrée Land and the Gauss Peninsula to the North.</p><br>
<h2>History</h2><br>
<p>This fjord was first surveyed and partially explored by the Second German North Polar Expedition 1869–70 and named Kaiser Franz Joseph Fjord for Franz Joseph, Emperor of Austria-Hungary, who had made substantial donations to the expedition.</p><br>
<p>Wollaston Foreland  is a peninsula in the NE Greenland National Park area, East Greenland.</p><br>
<h2>History</h2><br>
<p>This peninsula was named by William Scoresby in 1822 as a testimony of respect to William Hyde Wollaston. It was alo surveyed and explored by the Second German North Polar Expedition 1869–70 led by Carl Koldewey.</p><br>
<p>The Danish Sirius Dog Sled Patrol has its headquarters at Daneborg on the southeastern shore. The Zackenberg research station is situated further West, near Young Sound.</p><br>
<h2>Geography</h2><br>
<p>Wollaston Foreland is bounded in the north by the Lindeman Fjord and Albrecht Bay of Hochstetter Bay, in the east by the Greenland Sea, in the south by Young Sound and in the west by A. P. Olsen Land.</p><br>
<p>To the south and southwest across Young Sound lies large Clavering Island, close off northeast Sabine Island, and close off north Kuhn Island. Cape Wynn is the peninsula&#39;s easternmost point.</p><br>
<p>Wollaston Foreland is mountainous. Its highest point is the massive-looking 1444 m high Dombjerg, located in the western section near the isthmus. Other important mountains are Zackenberg, Kuplen, Nålene, Cardiocerasbjerg, Aucellabjerg, Murbjerg, Hühnerbjerg, Clark Bjerg and Herschell Bjerg.</p><br>
<h2>Bibliography</h2><br>
<p>Koldewey, Carl (1874) German Arctic Expedition of 1869-70, and Narrative of the Wreck of the Hansa in the Ice, London: Sampson Low, Marston, Low, & Searle</p><br>
<p>Mount Ena is a mountain peak of the Kiso Mountains range in the Chūbu region of Japan.</p><br>
<h2>Geography</h2><br>
<p>Mount Ena is 2,191 m in elevation. It is located on the border between Nakatsugawa in Gifu Prefecture, and Achi in Nagano Prefecture.</p><br>
<p>The mountain is on the list of landmark "100 Famous Japanese Mountains." The Kiso Mountains are the "Central Alps" of the scenic Japanese Alps group, located on central Honshu.</p><br>
<h2>Ascents</h2><br>
<h3>Hiking routes</h3><br>
<p>There are four hiking routes to the summit of Mount Ena, and are the:</p><br>
<p>Kuroisawa Route (黒井沢ルート)</p><br>
<p>Misaka Pass Route (神坂峠ルート)</p><br>
<p>Hirogawara Route (広河原ルート)</p><br>
<p>Maemiya Route (前宮ルート)</p><br>
<h3>Summit views</h3><br>
<p>The Japanese Alps ranges, Mount Ontake, Mount Haku, and part of Mount Fuji can be seen from the summit of Mount Ena.</p><br>
<p>Sabine Island  is an island to the northeast of Wollaston Foreland, previously known as Inner Pendulum Island. It is in the Northeast Greenland National Park area.</p><br>
<h2>Geography</h2><br>
<p>Sabine Island is 16 km long from Kap Neumayer in the north to Teddy Udkig in the south, and 14 km wide. The area measures 155.9 km², and the shoreline 59.8 km. The highest elevation is the 699 m high Keferstein. Other important peaks are Kronebjerg, Tafelbjerg and Søspidsen.</p><br>
<p>Together with an islet named Walrus Island (Hvalros Ø) off its southern point, and Little Pendulum Island located to the east, it constitutes the Pendulum Islands group. Numerous Inuit huts remain on the island.</p><br>
<p>There is also a small Sabine Island in Melville Bay, Northwest Greenland, as Mr. Sabine was also on the 1818 Ross expedition to these parts. That exposed islet was the site of a USA LORAN station in the post-war era.</p><br>
<h2>History</h2><br>
<p>The North East Greenland coast was colonized by Palaeo- and Neo-Eskimo groups in the past. The Inuit and their ancestors colonized and abandoned the area at least four times during the last four thousand years. There are remains of Inuit dwellings in Sabine Island that were first reported by Carl Koldewey during the Second German North Polar Expedition 1869–70.</p><br>
<p>Sabine Island was named Sabine Insel by Koldewey&#39;s expedition after the geophysicist General Sir Edward Sabine, who carried out pendulum gravimetric experiments on the island in 1823.</p><br>
<p>Sabine had been aboard the Clavering 1823 Arctic expedition, the only one to encounter living Inuit people in Northeast Greenland.</p><br>
<p>The Second German North Polar Expedition built a house at Germaniahafen on the south side. This station was later used by hunting expeditions.</p><br>
<p>From August 1942 to June 1943, the German meteorological expedition Unternehmen Holzauge under the command of Captain Hermann Ritter, with headquarters in Hansa Bay on the eastern side of the island, operated successfully on Sabine. It was discovered in March by the North-East Greenland Sledge Patrol, established by Greenland governor Eske Brun. In May, the station was bombed by USA aircraft from Iceland led by Colonel Bernt Balchen. In June, the surviving members of the German team were evacuated to Norway by air from a Dornier Do 18 seaplane launched from ship.</p><br>
<p>Andrée Land is a peninsula in King Christian X Land, East Greenland that is bounded by Kejser Franz Joseph Fjord, Isfjord and Geologfjord.</p><br>
<h2>History</h2><br>
<p>The peninsula was named by A.G. Nathorst on his 1899 expedition after Swedish Arctic explorer Salomon August Andrée, who had made an attempt to reach the North Pole by balloon in 1897. One of the aims of Nathorst’s 1899 venture was to search for traces of the lost Andrée&#39;s Arctic Balloon Expedition, whose fate was unknown until 1930, when it became known that Andrée had crash-landed on the pack ice and died on Kvitøya.</p><br>
<p>The region was later visited and accurately cartographed during Lauge Kocks expeditions to East Greenland.</p><br>
<h2>Geography</h2><br>
<p>Andrée Land is located about 100 km inland from the Foster Bay of the Greenland Sea. It is bound by Kaiser Franz Joseph Fjord in the southeast, and two branches of it, the Isfjord in the SW and the Geologfjord in the NE. The peninsula is attached to the mainland on its northwestern side, with the Gerard De Geer Glacier in its western boundary, and the Adolf Hoels Glacier and Nunatak Glacier in the north.</p><br>
<p>A number of valleys cut across the peninsula; the most important are the Grejsdalen in the middle, the Eremitdalen further north and the Rendalen in the west.</p><br>
<h3>Mountains</h3><br>
<p>Andrée Land is mountainous. The highest point is 2,360 m high Margaretatop, also known as Margarita Spids, located in the southern part. The Lacroix Mountains (Lacroix Bjerge) are a mountain range at the SW end rising above the Isfjord. Arnold Escher Land is a nunatak group to the NW of Andrée Land.</p><br>
<p>Some of the other noteworthy peaks are:</p><br>
<p>Aappalaatsiaq (1,998 m)</p><br>
<p>Agardh Bjerg (1,820 m)</p><br>
<p>Ajorpoq (1,498 m)</p><br>
<p>Alpebjerg (2,052 m)</p><br>
<p>Devil&#39;s Castle (Teufelsschloss) (1,303 m). Located at the SE end of Andrée Land on the fjord shore, opposite Cape Petersens, the NW extremity of Ymer Island.</p><br>
<p>Djævleborg (1,800 m)</p><br>
<p>Knivbjerg (1,987 m)</p><br>
<p>Marcia Bjerg (1,460 m)</p><br>
<p>Målebjerg (1,842 m)</p><br>
<p>Mørkebjerg (1,497 m)</p><br>
<p>Tårnfjeld (2,163 m)</p><br>
<p>The Chicago, Milwaukee, St. Paul & Pacific Railroad-Kittitas Depot is a railroad station in Kittitas, Washington that was built in 1909 by the Chicago, Milwaukee and St. Paul  as part of the railroad&#39;s Pacific Extension.</p><br>
<p>The depot is a rectangular, single-story, wood-frame building. It was built to serve the local community by shipping agricultural products. A small rail yard served the potato packing houses. In 1919, after the railroad electrified, an electric substation and operators houses were built adjacent to the depot. In 1974, the substation was razed, and the operators houses were sold to private individuals. After the railroad abandoned the Pacific Extension, the depot was taken over by the State of Washington and now is part of the Iron Horse State Park, a rails-to-trails initiative.</p><br>
<p>The depot was listed in the National Register because of its association with the Milwaukee Road and the development of railroads in Washington.</p><br>
<p>Long Lake is 5,625 acre lake in the USA state of Michigan. The lake is within two counities Alpena County and Presque Isle County in Northern Michigan. The lake is the 20th largest inland lake in Michigan.</p><br>
<p>The larger part of the lake is in Alpena Township, Michigan, with the southern shore approximately 7 mi from downtown Alpena along USA Highway 23, which continues along the eastern side of the lake. In Presque Isle County, the lake extends into Presque Isle Township and Krakow Township.</p><br>
<p>The lake is adjoined by an Alpena County park (including a day-use beach). Fish species include largemouth bass, smallmouth bass, northern pike, pumpkinseed sunfish, rock bass, yellow perch, walleye, and whitefish.</p><br>
<p>The name "Long Lake" is common among Michigan&#39;s 11,037 inland lakes which cover 1,305 square miles of inland water. This should not be confused with the 33 others (see Long Lake (Michigan), including the one in the vicinity of Long Lake Township, which is near Traverse City on the opposite side of the Lower Peninsula of Michigan.</p><br>
<p>Germania Land or Germanialand is a peninsula in northeastern Greenland. Despite the high latitude it is largely unglaciated.</p><br>
<h2>History</h2><br>
<p>This peninsula was named by Ludvig Mylius-Erichsen, leader of the Danmark expedition, to commemorate its survey by the Second German North Polar Expedition led by Carl Koldewey in 1869 on the vessel Germania and as a compliment to Alfred Wegener, the German member of the Danmark expedition.</p><br>
<p>In central Germania Land there is a cairn erected by the members of the Second German North Polar Expedition on 15 April 1870 in order to mark the farthest northern point they reached.</p><br>
<h2>Geography</h2><br>
<p>Germania Land is located in King Frederick VIII Land, in the Northeast Greenland National Park, between the Skaerfjord and Dove Bay. Store Koldewey island lies south of the southeastern point of the peninsula. The Musk Ox Mountains (Moskusoksefjeldene) are a hill range located east of Hvalrosodden, a small peninsula.</p><br>
<p>The Danmarkshavn weather station is on the southern shore of the Germania Land Peninsula. It was named by the 1906–08 Danmark Expedition after Danmark, the ship of the expedition which wintered there.</p><br>
<h2>Bibliography</h2><br>
<p>Koldewey, Carl (1874) German Arctic Expedition of 1869-70, and Narrative of the Wreck of the Hansa in the Ice, London: Sampson Low, Marston, Low, & Searle</p><br>
<p>Chadkirk Chapel is a redundant chapel near Romiley in the Metropolitan Borough of Stockport in Greater Manchester, England. It is recorded in the National Heritage List for England as a designated Grade II* listed building.</p><br>
<h2>History</h2><br>
<p>There are records of a chaplain at or maybe from Chadkirk in 1347. Constructed 170 years before the Reformation, this kirk (Scottish word for church) started its life as a Roman Catholic church. In time, the chapel fell into decay, passed through a succession of owners and was used as a stable. For a time it was used by Nonconformists who were ejected during the reign of Queen Anne. It again became neglected and was "in a ruinous condition" until in 1747 it was taken over once again by the Church of England and restored. Further repairs were carried out in 1761 and 1860. In 1876 there was a restoration when much of the furniture was removed. The Chapel was declared redundant in 1971 and was acquired by Bredbury and Romiley Urban District Council. In 1974 local government reorganisation abolished "urban districts" and the area was transferred to the newly created Stockport Metropolitan Borough Council. The chapel was restored in 1995 and is now open as a visitor attraction.</p><br>
<h2>Architecture</h2><br>
<p>The present building dates from the 16th century, although the south walls were rebuilt in 1747. It is a timber-framed building with a slate roof but most of the walls have been rebuilt in dressed stone. At the west end is a timber bell-cote with a pyramidal roof and a weather-vane. The south wall of the nave has two doors and two windows with semicircular heads. Above the west door is a gabled dormer window. The chancel has a semicircular-headed window. The east and north walls of the chancel retain their timber framing. At the east end is a window with a semicircular head.</p><br>
<p>Price Public Elementary School, now known as Price Public Community Center and Swift Museum, is a former African-American school in Rogersville, Tennessee. It currently serves as a community center.</p><br>
<p>The site of the school was dedicated to African-American education in 1868, when Alexander Fain, Jordan Netherland, Albert Jones and Nathaniel Mitchell bought the land "for the purpose of building a schoolhouse for the education of colored children." A schoolhouse was built and used until the early 1900s. The current building replaced it in 1922.</p><br>
<p>Price School operated until 1958, when it closed and its students were transferred to Swift High School, which was converted from a high school to a grade K-12 school. When integration took place in Rogersville, during the 1960s, the city&#39;s African-American elementary school students were transferred to Rogersville City School, also a K-8 institution. The Price School building was subsequently used as a cannery, a community center, and a storage building, then was abandoned and became run-down.</p><br>
<p>The school was listed on the National Register of Historic Places in 1988.</p><br>
<p>The building underwent a restoration beginning in the mid-1990s as a result of cooperative efforts between the town, the local African-American community, the local American Legion Auxiliary, the Chamber of Commerce, the Rogersville Heritage Association, and other civic organizations.</p><br>
<p>The Rogersville Historic District is a historic district in Rogersville, Tennessee, the county seat of Hawkins County. It is both a local historic district and a National Register of Historic Places historic district.</p><br>
<p>The local historic district established by the Town of Rogersville to safeguard, preserve, and protect hundreds of unique and historically significant structures in and around the towns downtown area. It comprises numerous neighborhoods and business areas, with architecture and significant historical events occurring throughout the history of the town, since its settlement by Davy Crocketts grandparents in 1775.</p><br>
<p>The street plan of the core of the district, which centers on Rogersvilles commercial and governmental hub, was designed by the towns founder, Joseph Rogers, when he petitioned the North Carolina General Assembly to establish a town at Hawkins Court House in 1786.</p><br>
<p>The local historic district is administered by the Town of Rogersville&#39;s Historic Preservation Commission, a governmental body.</p><br>
<p>It includes numerous historically significant structures, including:</p><br>
<p>Hale Springs Inn, c. 1824</p><br>
<p>Hawkins County Courthouse, c. 1836</p><br>
<p>Overton Lodge, c. 1840</p><br>
<p>The entire Rogersville Historic District is listed on the National Register of Historic Places.</p><br>
<p>The Newark Earthworks in Newark and Heath, Ohio, consist of three sections of preserved earthworks: the Great Circle Earthworks, the Octagon Earthworks, and the Wright Earthworks. This complex, built by the Hopewell culture between 100 AD and 500 AD, contains the largest earthen enclosures in the world, being about 3,000 acres in extent. Today, the preserved site covers 206 acres, and is operated as a state park by the Ohio History Connection. A designated National Historic Landmark, in 2006, the Newark Earthworks was also designated as the "official prehistoric monument of the State of Ohio."</p><br>
<p>This is part of the Hopewell Ceremonial Earthworks, one of 14 sites nominated in January 2008 by the USA Department of the Interior for potential submission by the US to the UNESCO World Heritage List.</p><br>
<h2>History</h2><br>
<p>Built by the pre-European contact Hopewell culture between 100 AD and 500 AD, the earthworks were used as places of ceremony, social gathering, trade, worship, and honoring the dead. However, the primary purpose of the Octagon earthwork itself was believed to have been scientific. The Newark Earthwork site is the largest surviving Hopewell earthwork complex in North America. The culture built many earthen mounds. Over decades, they built the single largest earthwork enclosure complex in the Ohio River Valley. The earthworks cover several square miles. Scholars have demonstrated that the Octagon Earthworks comprise a lunar observatory for tracking the moon&#39;s orbit during its 18.6-year cycle.</p><br>
<h2>Great Circle Earthworks</h2><br>
<p>The 1,054 ft wide Newark Great Circle is one of the largest circular earthwork in the Americas, at least in construction effort. A 5 ft deep moat is encompassed by walls that are 8 ft high; at the entrance, the dimensions are even more grand.</p><br>
<p>Researchers have used archaeogeodesy and archaeoastronomy to analyze the placements, alignments, dimensions, and site-to-site interrelationships of the earthworks. This research has revealed that the prehistoric cultures in the area had advanced scientific understanding as the basis of their complex construction.</p><br>
<p>Today, the Great Circle Earthworks are preserved in a public park in Heath.</p><br>
<h2>Octagon Earthworks</h2><br>
<p>Fifty acres total, the Octagon Earthworks consists of an Observatory Mound, Observatory Circle, and the interconnected Octagon span nearly 3,000 ft in length. It has eight 550 ft-long walls, from 5 ft to 6 ft high. The Octagon Earthworks are joined by parallel walls to a circular embankment enclosing 20 acres.</p><br>
<p>In 1982 researchers from Earlham College in Richmond, Indiana concluded that the complex was a lunar observatory, designed to track motions of the moon, including the northernmost point of the 18.6-year cycle of the lunar orbit. When viewed from the observatory mound the moon rises at that time within one-half of a degree of the octagon&#39;s exact center. The earthwork is twice as precise as the complex at Stonehenge (assuming Stonehenge is an observatory, which is a disputed theory).</p><br>
<p>From 1892 to 1908, the state of Ohio used the Octagon Earthworks as a militia encampment. Immediately after this, the Newark Board of Trade owned the property, until 1918. In 1910, they leased the property to Mound Builders Country Club (MBCC), which developed the site as a golf course. As a result of a Licking County Common Pleas Court case, a trustee was named to manage the property from 1918 to 1933.</p><br>
<p>In 1997 the Ohio Historical Society (now the Ohio History Connection) signed a lease until 2078 with the country club. MBCC maintains, secures, and provides some public access to the land. Some citizens believe the country club is an inappropriate use of the sacred site. There has been increasing public interest in the earthworks. Activists have pressed for more public access to the site to witness the moonrise, which observance was planned in the design and construction by the original native builders.</p><br>
<h2>Wright Earthworks</h2><br>
<p>The Wright Earthworks consist of a fragment of a geometrically near-perfect square enclosure and part of one wall that originally formed a set of parallel embankments, which travelled from the enclosure to a large oval yard. The Newark square&#39;s sides formerly ranged from about 940 ft to 940 ft in length, enclosing a total area of about 20 acres.</p><br>
<p>The Wright Earthworks are named in honor of Mrs. Frances Rees Wright, who donated the site to the Ohio Historical Society in 1934.</p><br>
<p>Dinglishna Hill is a hill located East of Mount Susitna, in the Matanuska-Susitna Valley of South Central Alaska. It is also the name of the Dinglishna Hills subdivision of the Matanuska-Susitna Borough, Alaska.</p><br>
<h2>History</h2><br>
<p>Tanaina Indian name reported in 1958 by USGS.</p><br>
<h3>Etymology</h3><br>
<p>Dgelishla or Dghelishla in Dena&#39;ina meaning "Little Mountain" is transliterated as "Dinglishna".</p><br>
<h2>Description</h2><br>
<p>Dinglishna Hill is on W bank of Alexander Creek, 28 mi north west of Anchorage, Cook Inlet Low.</p><br>
<h2>Location</h2><br>
<p>Dinglishna Hill is a hill located East of Mount Susitna, West of Alexander Creek and the big Susitna River, South-West of Susitna, and North of Alexander in the Matanuska-Susitna Valley of South Central Alaska.</p><br>
<p>It is also the name of the Dinglishna Hills subdivision of the Matanuska-Susitna Borough, Alaska.</p><br>
<h2>Terrain</h2><br>
<p>The elevation of Dinglishna Hill is 479 ft above mean sea level. The hill slopes down gradually until it reaches Alexander Creek near the confluence with the big Susitna River.</p><br>
<h2>Vegetation</h2><br>
<p>The hill and its surroundings are vegetated with birch, spruce and low lying shrubs. The soil in the area is well-drained.</p><br>
<p>Bangarh  is the historical place situated in Gangarampur, West Bengal, India. Bangarh was the ancient city which was the administrative centre of Kotivarsha Vishaya , itself part of the wider administrative unit of Pundravardhana Bhukti, which had Mahasthangarh as its capital in the period of Chandras, Varmans and Senas. After the Senas were defeated by the Muslims under Bakhtiar Khilji, Devkot was established as their capital were Bakhtiar breathed his last</p><br>
<h2>History</h2><br>
<p>The earliest mentions about the Kotivarsha town are found in the Vayu Purana (XXIII,209) and the Brihat Samhita (XI,II). Lexicographers, Hemchandra (the Abhidhanachintamani IV,977) and Purushottama (in his Trikandashesha) have mentioned the city by several names – Uma(Usha?)vana, Banapura, and Shonitapura. Sandhyakara Nandi in his Ramacharita described at length about the temples and the lakes of the city. The ruins of the city are found in Bangarh, which is located at Gangarampur city, about 45 km south of Balurghat city, in Dakshin Dinajpur district of West Bengal state in eastern India. It has variously thought of as part of Pundravardhana or Rarha regions. There was a Brahmin densities at Devikota.</p><br>
<p>Muslim rule was first established in Bengal in 1204 by Bakhtiyar Khilji. The kingdom was called Lakhnawati or Lakhnauti. The capital was located sometimes at Lakhnawati and sometimes at Devkot. Bakhtiyar Khilji died at Devkot in 1205-06, possibly murdered by Ali Mardan, who was governor of Naran-Koh, although this account is deemed erroneous by most Historians and it is established that Bakhtiyar died as a result of the physical wounds and mental trauma he endured from his unsuccessful trip to Tibet which was essentially cut short in northern Assam.</p><br>
<h2>Excavations at Bangarh</h2><br>
<p>The earliest excavations at Bangarh was carried out by a team led by K.G. Goswami during 1938-41. Located on the bank of the Punarbhaba, the excavated site reflects its urban character. The site has its core in the form of a citadel surrounded by mud ramparts (area about 25 hectares) which dates from the earliest phase of the site.The earliest phase remains uncertain, as the excavations could not reach the natural soil. The citadel area revealed five cultural phases dating from the time of the Mauryas to the medieval period. The initial phase (the Mauryan period) indicates that the city had a modest beginning in which it had probably a mud rampart wall. It was only in the following phase (the Kushana period, 200 BCE - 300 CE) a brick built wide rampart wall is found with drains, cesspits and residential buildings made of burnt bricks of a very large size, showing distinct signs of prosperity and burgeoning urbanism. The excavated materials of the Gupta period are not comparable with the richness and diversity of those belonging to Kushana cultural phase. Though the late Gupta phase of Bangarh is marked by decadence, particularly in terms of building activities, the Pala period (mid 8th century -12th century), in sharp contrast, indicates a picture of efflorescence. Rampart walls, compound walls, residential quarters, temples with ambulatory path and its enclosing walls, damp proof granaries, bathrooms, drains and ring wells suggest a prosperous condition of the city.</p><br>
<p>The Bullard-Hart House in Columbus, Georgia was built during 1887-90 for Dr. William L. Bullard, Columbus physician and pioneer ear, eye, nose, and throat specialist.</p><br>
<p>The house is a splendid example of Second Empire Victorian architecture. It was designed by architect L. E. Thornton of New York.</p><br>
<p>The Bullard family lived here for 90 years. Their guests included President Franklin D. Roosevelt and Generals George Patton and George Marshall who dined on "Country Captain," a popular regional dish originated by the family cook, Arie Mullins.</p><br>
<p>The house was listed on the USA National Register of Historic Places in 1977.</p><br>
<p>It was painstakingly restored in 1978 by new owners, Dr. and Mrs. Lloyd Sampson.</p><br>
<p>The Pocumtuck Range, also referred to as the Pocumtuck Ridge, is the northernmost subrange of the Metacomet Ridge mountain range of southern New England. Located in Franklin County, Massachusetts, between the Connecticut River and the Deerfield River valleys, the Pocumtuck Range is a popular hiking destination known for its continuous high cliffs, scenic vistas, and microclimate ecosystems.</p><br>
<h2>Geography</h2><br>
<p>The range, 11 miles (18 km) long by 1.75 miles (2.8 km) wide at its widest point,</p><br>
<p>includes, from south to north, Sugarloaf Mountain of Deerfield; a central high ridge most often called Pocumtuck Ridge; and Rocky Mountain (sometimes called Greenfield Ridge) of Greenfield. Notable peaks include, from south to north:</p><br>
<p>South Sugarloaf Mountain, 652 ft, a butte-like peak at the south end of the Pocumtuck Range, well known for its historic summit automobile road and abrupt butte-like cliffs overlooking the Connecticut River valley south.</p><br>
<p>North Sugarloaf Mountain, 791 ft, looms above South Sugarloaf with ledges facing south and west.</p><br>
<p>Pocumtuck Rock, 846 ft, the sandstone high point on the 2-mile (3 km) long cliffs of the Pocumtuck Ridge which rise 500 ft above Interstate 91 and the rural Deerfield River Valley to the west.</p><br>
<p>Trap Rock Ledge, 452 ft, a trap rock overlook on the east side of Pocumtuck Ridge.</p><br>
<p>Sachem Head, 452 ft, a popular, exposed overlook at the south end of Rocky Mountain.</p><br>
<p>Poet&#39;s Seat Tower, 492 ft, high point of Rocky Mountain, overlooking Greenfield.</p><br>
<p>Canada Hill, 338 ft, the steep northern prominence of Rocky Mountain at the confluence of the Connecticut River and Falls River, prominent from both Greenfield and from the Connecticut River mill village of Turner&#39;s Falls, Massachusetts to the east.</p><br>
<p>The Deerfield River cuts between Rocky Mountain and Pocumtuck Ridge just before merging with the Connecticut River.</p><br>
<p>The Pocumtuck Range is located entirely in Deerfield and Greenfield. The Metacomet Ridge, of which it is a part, continues north as a series of low sedimentary hills and dwindling trap rock outcrops to just two miles south of the Vermont and New Hampshire borders in Northfield, Massachusetts. South of Sugarloaf Mountain, the Metacomet Ridge virtually disappears into low, scattered rises and flat plains of sedimentary rock before ascending again as the prominent trap rock Holyoke and Mount Tom Ranges nine miles south.</p><br>
<h2>Origin of the name</h2><br>
<p>Pocumtuck (Pocumtuc) was the name of a now extinct tribe of Native Americans who lived in the area prior to 1800. According to stories ascribed to the tribe, Pocumtuck Ridge and Sugarloaf Mountain were the remains of a giant beaver killed by the giant spirit Hobomock (the same spirit who diverted the course of the Connecticut River in central Connecticut and was cursed to sleep forever as the Sleeping Giant mountain formation). The Pocumtucks allegedly believed that the beaver lived in an enormous lake that once occupied the Connecticut River Valley:</p><br>
<p>The Great Beaver, whose pond flowed over the whole basin of Mt. Tom, made havoc among the fish and when these failed he would come ashore and devour Indians. A pow-wow was held and Hobomock raised, who came to their relief. With a great stake in hand, he waded the river until he found the beaver, and so hotly chased him that he sought to escape by digging into the ground. Hobomock saw his plan and his whereabouts, and with his great stake jammed the beavers head off. The earth over the beavers head we call Sugarloaf, his body lies just to the north of it.</p><br>
<p>A number of different versions of this story exist, all of them similar. There may be some scientific truth to the account. The lake described in the tale is very reminiscent of the post-glacial Lake Hitchcock which occupied the Connecticut River Valley from Burke, Vermont to New Britain, Connecticut 15,000 years ago.Raymo, Chet and Maureen E. Written in Stone: A Geologic History of the Northeastern United States. Globe Pequot, Chester, Connecticut, 1989.</p><br>
<p>Around this time, a giant beaver species (Castoroides ohioensis) thrived from the post-glacial front to as far south as Florida. The animals were as large as black bears, weighed up to 450 lbs., and had teeth the size of bananas. A similar legend about the killing of a giant beaver by a helper-spirit and the subsequent transformation of the corpse into a landform occurs among the native Mi&#39;kmaq people of Nova Scotia (see Glooscap).</p><br>
<h2>Geology and ecosystem</h2><br>
<p>The Pocumtuck Range hosts a combination of microclimate ecosystems unusual to the region. Eastern red cedar, a dry-loving species, clings to the barren edges of cliffs. Backslope plant communities tend to be similar to the adjacent upland plateaus and nearby Berkshires, containing species common to the northern hardwood and oak-hickory forest ecosystem types. Eastern hemlock crowds narrow ravines, blocking sunlight and creating damp, cooler growing conditions with associated cooler climate plant species. Talus slopes are especially rich in nutrients and support a number of calcium-loving plants uncommon in the region. Miles of cliffs make ideal raptor habitat, and the range is an important seasonal raptor migration corridor. Thirty-seven species of fern can be found on the range, making it one of the richest ecosystems of fern diversity in the Commonwealth of Massachusetts. The range also supports extensive populations of whorled pogonia, a plant on the Massachusetts Environmental Protection Agency&#39;s watch list.</p><br>
<p>The Massachusetts Audubon Society considers the Rocky Mountain section of Pocumtuck Ridge "exceptionally rich in its diversity of species, especially during migration...an important area for breeding birds, and wintering individuals."</p><br>
<h2>Recreation and Conservation</h2><br>
<p>Seventy percent of the ridgeline route traversed by the 20 mi Pocumtuck Ridge Trail has been conserved as state, municipal, or non profit holdings, or as private land under conservation easement. The rest of the ridgeline, and much of the slopes of the mountain, remain in the private domain. The trail begins on South Sugarloaf and traverses the ridge to Poet&#39;s Seat.</p><br>
<p>A network of smaller marked and unmarked trails also crisscross the range. Sugarloaf Mountain, at the southern end of the range, is managed as the Mount Sugarloaf State Reservation, with an observation tower and automobile toll road, open in season. Several trails climb to the summits. Poets Seat and the adjacent parklands on Rocky Mountain are managed by the City of Greenfield. Poets Seat Tower Park features a 1912 sandstone observation tower named in honor of local poet Frederick Goddard Tuckerman. The annual Fourth of July fireworks celebration takes place at Poet&#39;s Seat. The tower is open seasonally via a quarter-mile walk from a ridgetop trailhead or via auto road (in season). An observation platform at the abrupt ledge of Sachem Head is accessible via the same trailhead. Eaglebrook School, a boarding school for boys grades six to nine, runs the chairlift-served Easton Ski Area on the west side of Pocumtuck Ridge (closed to the public). A defunct Eaglebrook ski area is located to the north. Another defunct ski area, once operated by Deerfield Academy, is located on the east side of the ridge.</p><br>
<p>The Pocumtuck Range is most threatened by development and quarrying. The Massachusetts Department of Conservation and Recreation and several local conservation non-profits have made conservation of the range a priority.</p><br>
<p>First Church of Christ, Scientist was a Prairie School church building located at 412 West Main Street, in Marshalltown, Iowa, United States. Designed by noted architect, Hugh M.G. Garden, it was once on the National Register of Historic Places, but was bulldozed in August, 1985, and was later removed from the National Register.</p><br>
<h2>National register listing</h2><br>
<p>First Church of Christ, Scientist ** (added 1998 - Building - #79000915)</p><br>
<p>412 W. Main St., Marshalltown</p><br>
<p>Historic Significance: Architecture/Engineering</p><br>
<p>Architect, builder, or engineer: Garden, Hugh M.G.</p><br>
<p>Architectural Style: Prairie School</p><br>
<p>Area of Significance: Architecture</p><br>
<p>Period of Significance: 1900-1924</p><br>
<p>Owner: Private</p><br>
<p>Historic Function: Religion</p><br>
<p>Historic Sub-function: Religious Structure</p><br>
<p>Current Function: Religion</p><br>
<p>Current Sub-function: Religious Structure</p><br>
<p>The former First Church of Christ, Scientist, located in Davenport, Iowa, United States, is an historic building that was added to the National Register of Historic Places in 1984. It is now the Harvest Time Family Worship Center.</p><br>
<h2>History</h2><br>
<p>First Church was established in Davenport in 1892 by 16 practitioners as a branch of the mother church in Boston. They built this building, which was designed by the prominent Davenport architectural firm of Clausen & Clausen, in 1912. They opened a Christian Science Reading Room downtown. First Church moved in the 1970s to a new facility on Fairhaven Road in Davenport.</p><br>
<p>The Harvest Time Family Worship Center was founded by the Revs. James and Cecelia Lee as the Pentecostal Deliverance Church in 1972. It was located in the 1500 block of Fillmore Street at the time. The congregation moved to this location in 1980.</p><br>
<h2>Architecture</h2><br>
<p>The structure is a severe example of the Neoclassical style. The cross plan of the building is the only religious symbolism employed. It is very similar in that way to the original St. Anthony&#39;s Catholic Church (1836) downtown. The main facade is dominated by the tetrastyle temple front with columns in antis that follow the Doric order. The main entrance into the church is recessed behind the tetrastyle "screen" and it is surmounted by a fanlight. The entry itself is made up of three openings and follows a Palladian motif. The central opening features a rounded arch. At the crossing in the center of the structure is a polygonal belvedere. The wood and concrete structure is covered with stucco.</p><br>
<p>The Bishop Portier House is a historic residence in Mobile, Alabama, United States. It sits diagonally across from the Cathedral of the Immaculate Conception, and faces Cathedral Square. It is owned by the Roman Catholic Archdiocese of Mobile. The house, built c. 1834, is one of Mobile&#39;s best surviving examples of a Creole cottage with neoclassical details. It was listed on the National Register of Historic Places on February 26, 1970 and subsequently was added to the Historic Roman Catholic Properties in Mobile Multiple Property Submission also.</p><br>
<h2>History</h2><br>
<p>The house is named for Michael Portier, Mobile&#39;s first Roman Catholic bishop, who made this his home from 1834, until his death in 1859. The house was designed by Claude Beroujon, a seminarian architect and nephew of Portier. Four subsequent bishops resided here until 1906. Fr. Abram Ryan, poet-priest of the South, occupied the northwest corner room on the second floor from 1870, until 1877. The residence was restored by the archdiocese in 1958, and again in 2007. In 1970, it was placed on the National Register of Historic Places.</p><br>
<h2>Description</h2><br>
<p>The structure is frame with clapboarding, and plastered gallery. It is one and one-half stories, with a square plan, and a center hall running from front to rear. It has a gabled roof encompassing full-length galleries, front and rear, on slender columns. There are three ornate dormers with classical detail. The center entrance is framed by pilasters, entablature, transom, and side lights.</p><br>
<p>Gregory Chapel is one of the high points of the fells on the border between Cumbria and North Yorkshire.</p><br>
<p>The summit is marked by a nearby sheep shelter and an unusual and conspicuous cairn - taller and more rectangular than most others locally. (This may, perhaps, be the origin of the curious name "chapel"?)</p><br>
<p>The main rock in the area is limestone, with Millstone Grit outcrops on the tops. There are fine views over to Wild Boar Fell and Swarth Fell 5 km to the west, across the dale of Mallerstang.</p><br>
<p>Hill walkers seem to prefer to give it the name Archy Styrigg; although Ordnance Survey maps show this name along the small plateau at about 680 m elevation to the southwest of the summit, leading over Mallerstang Edge. (This would fit the Norse name, characteristic of this area: sty=track or path, rigg=ridge: i.e. path along a ridge).</p><br>
<p>It is classified as a Nuttall and sub-Hewitt, but it has a relatively small prominence, having several other high points nearby, and hardly merits being described as a peak. This high, boggy ground is really one great plateau which rarely drops much below 600 m (2000 ft) between Mallerstang Edge and Great Shunner Fell, 5.4 km to the south-east.</p><br>
<p>Gregory Chapel is one of the three high points of Mallerstang Edge, the others being High Seat 1.04 km almost due north, and Hugh Seat 1.26 km SSE. They mark the eastern border of the Parish of Mallerstang, Cumbria - which is also the county border between Cumbria and North Yorkshire.</p><br>
<h2>Walking the Parish Bounds</h2><br>
<p>This extract from the 1811 report on the walking of the parish bounds, lists the landmarks to be visited in this area as:</p><br>
<p>.12 As heaven water deals, to the south end of High seat</p><br>
<p>13 Thence over little Sleddle head to Gregory Chappell</p><br>
<p>14 Thence along Gregory band to a hurrock of stones</p><br>
<p>15 Thence to the height of Hugh Seat Morvill</p><br>
<p>16 Thence as heaven water deals, to the Skarth of Skaiths...</p><br>
<p>The charming term "as heaven water deals" means following the course of a beck downstream.</p><br>
<p>The parish bounds were last walked in July 2006</p><br>
<p>Doukades  is a village and a community in the northwestern part of the island of Corfu. It is located in the municipal unit of Palaiokastritsa. In 2011 its population was 627 for the village and 721 for the community, including the village Papathanatika. Hills dominate the area.</p><br>
<h2>Population</h2><br>
<h2>History</h2><br>
<p>According to I. Bounia, the name of the settlement came from its first inhabitants who bore the name Doukas (Δούκας, meaning duke). The earliest written reference to Doukades is a notary writing from 1616. Of interest are the restored stone mansion of the family Theotokis, the Venetian type "Sagrado" of Kouartano, and the building of the elementary school at the entrance of the village.</p><br>
<p>Doukades was characterized as a traditional settlement with the law of October 19, 1978 No. 594 IV / November 13, 1998 (Codical statistics, number 22.1.137.01).</p><br>
<p>Orange Center Historic District is a historic district encompassing the historic civic, commercial, and industrial heart of Orange, Massachusetts in the United States. It was listed on the National Register of Historic Places in 1989.</p><br>
<h2>Description and history</h2><br>
<p>The area that is now the center of Orange was settled about 1785, when a bridge was built across the Millers River, which flows through it in a westerly direction toward the Connecticut River. The town grew in the first half of the 19th century as an industrial area, and its growth increased substantially with the arrival of the railroad in 1846. It became widely known in the second half of the 19th century for the manufacture of sewing machines. The town&#39;s economy declined during the Great Depression, and has been at a lower ebb since then.</p><br>
<p>The historic district is roughly linear, extending north-south along North and South Main Streets from School Street in the north to River Street on the south side of the Miller River. It extends for a short distance along East and West Main Streets. Included in its roughly 12 acre are 37 historically significant buildings, most of which are commercial brick or wood-frame buildings in a variety of styles. Also included are the town hall (built 1868), two churches, railroad-related infrastructure including a surviving freight house, and the Grand Army of the Republic Hall. At the northern end of North Main Street are a few period residences, including the ornate Italianate French House that now serves as the home to the local historical society.</p><br>
<p>Wilkins Peak is a small mountain located in Sweetwater County, Wyoming, between the cities of Green River and Rock Springs. It is primarily used for radio and television station transmitters, but it also serves radio needs of the FAA, EMS, and local businesses such as Questar Gas. In 2003, a tower on the peak was knocked down by a vehicle delivering propane to customers. The tower was owned by Wyoming Public Radio and was serving the local area with programming from National Public Radio. There are numerous access roads to the peak and it is not gated and open year-round, weather permitting. Along with the radio uses, the mountain is also a popular location for mountain biking and hiking. The mountain contains geology typical of its location in southwestern Wyoming.</p><br>
<h2>Geology</h2><br>
<p>Along with other mountains in southwestern Wyoming, Wilkins Peak is part of the Green River Formation, a formation of the intermontane Lake Gosiute environment during the Eocene epoch. Similar to its neighboring Aspen Mountain, Wilkins Peak is part of the Rock Springs Uplift, and some of the largest oil shale and trona beds in the region are located near the mountain. Wilkins Peak also has its own distinct segment of the Green River Formation, which is known as the Wilkins Peak Formation.</p><br>
<p>The peak itself is 7,650 ft in elevation and is located 8.18 mi from Rock Springs, Wyoming and 6.3 mi from Green River, Wyoming.</p><br>
<h2>Radio and television uses</h2><br>
<p>Wilkins Peak holds radio towers for several FM radio and television stations. Stations include KYCS (95.1 FM) and its sister stations KFRZ (92.1 FM) and KZWB (97.9 FM). Also on the mountain is the tower for the station KTME 89.5, which signed on the air in September 2010. KTME is an affiliate of Pilgrim Radio. KREO 93.5 is the newest station on the peak.</p><br>
<p>Several television translators transmit their signals from two small towers located in the center of Wilkins Peak. Additionally, the religious television network TBN has a translator known locally as K35CN, broadcasting from the mountain. Prior to 2009, K22BK, the local PBS television translator, carried its signal from Wilkins Peak. K22BK was moved across the interstate to White Mountain to the same tower as its digital counterpart. In late 2009, a new television station signed on the air from the peak. It is known as K33IX-D on channel 33 (UHF) and carries programming from EICB TV, a Christian religious broadcast and production company, based in Cedar Hill, Texas. K35CN and K22BK have been off the air since the digital television transition in the year 2009.</p><br>
<h3>FM translators</h3><br>
<p>Among high powered FM radio stations, Wilkins Peak is also currently host to three lower powered FM translators. K205FE carries a Gospel format on 88.9 FM. K285FG retransmits programming from AM station KUGR on 104.9 FM. Finally, K290BJ carries programming from KZWB 97.9 FM.</p><br>
<h3>Other radio related uses</h3><br>
<p>Wilkins Peak also has repeater towers for local police, fire, and EMS services. The emergency radio repeaters on the mountain are used in conjunction with other repeaters located on nearby Aspen Mountain and Mansface Hill.</p><br>
<p>In September 2003, a commercial truck delivering propane to customers on the peak knocked down the then-existent KUWZ tower after the vehicle&#39;s brakes failed. The collapse of the tower knocked out power to the mountain for several hours, and while KUWZ borrowed space from neighboring towers for several months thereafter, the station ultimately relocated its transmitter to nearby Aspen Mountain.</p><br>
<h2>Accessing the peak</h2><br>
<p>Wilkins Peak is not gated, and it can be reached via an unpaved road known as Wilkins Peak Road that starts on USA Route 191 southwest of Rock Springs, Wyoming. The mountain can also be accessed via another unpaved road that begins in the Scott&#39;s Bottom Nature Area in Green River, Wyoming. The peak is accessible year-round, weather permitting. The Green River access road is in worse shape than the Rock Springs side, and it has several road hazards such as steep grades, poor grading, and off-road vehicle traffic. Along with serving radio needs, the peak also is a popular hiking and mountain biking location in the area. There are many smaller roads and trails that spring from the peak that offer varied degrees of challenge.</p><br>
<p>Pressmens Home was a community and the headquarters for the International Printing Pressmen and Assistants Union of North America from 1911&ndash;1967. The facilities provided on the unions campus, in Hawkins County, Tennessee near Rogersville, included a trade school, a sanitarium, a retirement home, a hotel, a post office, a chapel, a hydroelectric power production plant, and other facilities designed to make it a self-sufficient community.</p><br>
<p>It is listed on the National Register of Historic Places as a historic district.</p><br>
<h2>History</h2><br>
<p>Pressmens Home was the brain-child of George L. Berry, who grew up near the site in Hawkins County, Tennessee. After he became president of the Pressmens Union, he convinced union leaders to purchase the Hale Springs Resort, a mineral springs retreat. The buildings from the resort formed the core of Pressmen&#39;s Home around which later facilities were constructed.</p><br>
<p>As the union grew, so did Pressmens Home, adding larger and more elaborate facilities. In its heyday, Pressmens Home was a self-sufficient town that even provided its own electricity (several years before the Tennessee Valley Authority did the same for the rest of Hawkins County).</p><br>
<p>Beginning in the mid-1960s pressure from competing unions to lobby the USA federal government was beginning to convince leaders of the union that their location in rural East Tennessee was becoming detrimental to the interests of the Union. The Union announced it was moving its headquarters in 1967; lack of funding and merger with other printing unions led to the closure of Pressmen&#39;s Home as a retirement facility for union members in 1969.</p><br>
<p>Since the Union left, several schemes have been proposed to revive the site, including tourist resort, retirement community, and even a state penitentiary. Today the only active project is a golf course and country club that sometimes operates a restaurant. Buildings on the property have fallen into disrepair; several have burned down due to fires that started by accident or by arson.</p><br>
<h2>Post office</h2><br>
<p>Pressmens Home had a Post office from 1914–1971. It closed three years after the Union moved. A second post office operated in Pressmens Home as Camelot from 1971-1975.</p><br>
<h2>Major facilities</h2><br>
<h3>Administration Building</h3><br>
<p>The Administration Building was built in 1912 and was the original location of the Trade School. After new Trade School facilities were built in 1947, the building housed the executive offices of the Union&#39;s International president and secretary-treasurer. The Membership Records Department, the Accounting Department, the Service Bureau and the editorial offices were also housed in the building.</p><br>
<p>The building was abandoned after the Union left Pressmen&#39;s Home in 1969.</p><br>
<h3>Home Building</h3><br>
<p>The Home Building was built in 1911. It was under construction when the Union moved its headquarters to Pressmen&#39;s Home after purchasing the Hale Springs Resort.</p><br>
<p>It was built to house the visitors that had formerly visited the Hale Springs (which were believed to have medicinal qualities, due to the high sulphur concentrations in the spring water). The building was home to many of the International officers while they stayed at Pressmen&#39;s Home. After a hotel was completed in 1926, the building became known as simply "The Home," and it was used as an apartment complex for full-time residents. The Home was equipped with a kitchen, dining room, pool room, and other amenities.</p><br>
<p>The building fell into disrepair after the Union left Pressmen&#39;s Home; today it stands in ruins.</p><br>
<h3>Tuberculosis sanitorium</h3><br>
<p>The Sanatorium was built in 1916. In the early years of printing it was thought that exposure to printer&#39;s ink was a cause for tuberculosis. The Union was interested in the welfare of its members, and so the hospital was completely staffed, adequately equipped, and ideally situated for combating the deadly disease within the means of the technology of the times.</p><br>
<p>Union members who contracted the disease could come to Pressmens Home and receive care at no charge. Many who died from the disease are buried in the cemetery at Pressmens Home.</p><br>
<p>The building was demolished in 1962, to make way for other facilities before the Union left.</p><br>
<h3>Hotel Pressuaina</h3><br>
<p>In 1926, a four-storey hotel was built to accommodate Union members and their families that came to Pressmen&#39;s Home to train at the Trade School.</p><br>
<p>The hotels facade was made from sandstone removed from a quarry located on the premises. Inside the hotel, the lobby had a beautiful tile floor and an adjacent reading room. Home-cooked meals were prepared for the hotels guests, largely from on-site facilities that included a dairy farm for milk, chickens for eggs and poultry, a large vegetable garden, and hog lot for pork. The guest rooms were appointed with iron beds and dressers.</p><br>
<p>The hotel was destroyed in October 1994 by arson.</p><br>
<h3>Memorial Chapel</h3><br>
<p>The Memorial Chapel was built in 1926 as a non-denominational church dedicated to the memory of union members who died in World War I. Later, the Chapel&#39;s dedication was expanded to include all people who served in United States and Canadian military service since that time.</p><br>
<p>The chapel was designed by architect John Sheridan in the Italianate style and was built of native sandstone. It had stained glass windows from Louis Comfort Tiffany and a fresco painting on its ceiling. At the time of its construction, it was thought to be the only church owned by a labor union. Outside the chapel, in a garden, stood the printing press upon which the design of the union&#39;s logo was based.</p><br>
<p>George L. Berry, the president of the union and founder of Pressmen&#39;s Home, was interred in a mausoleum near the chapel. Both the chapel and the mausoleum still stand today, however, Berry and his wife’s remains, have been relocated to the town cemetery in Rogersville.</p><br>
<h3>Trade school building</h3><br>
<p>The Trade School building was built in 1948. It was the cornerstone of the educational and training program at Pressman&#39;s Home.</p><br>
<p>The school housed over $500,000 (more than $5.4 million in 2007) in presses and equipment. The school provided training in letterpress, gravure, and offset presses, ink mixing, camera, stripping, platemaking, color separation, and bindery operations. All of the equipment was provided to Pressman&#39;s Home by the manufacturer on a loan basis.</p><br>
<p>This trade school was an attempt by the Union to set itself apart from its union competitors. Trainees were required to have been in the union for five years, however many people from the Hawkins County area were allowed to train at the school at no charge without any experience.</p><br>
<p>Leslie Dam is located ten kilometres from Warwick Central Business District in Queensland, Australia. Freshwater fishing and water sports facilities are available.</p><br>
<p>The dam was named after Patrick Leslie (1815–1881), an early settler in the region and the first person to buy land in Warwick.</p><br>
<p>SunWater is undertaking a dam spillway capacity upgrade program to ensure a consistently high level of safety for the dams under their control, including the Leslie. The spillway will be upgraded in the longer term.</p><br>
<h2>History</h2><br>
<p>The dam was extended in 1986, increasing capacity by 100%. The dam&#39;s highest level was reached on 12 September 1988 when waters in the dam peaked at 20 cm above the spillway. The next highest level was 13 cm above the spillway on the 28 May 1990. On 11 February 1995, the dam reached its lowest level ever of 3% capacity.</p><br>
<p>On the night of 5 January 2011, the dam spilled for the first time in more than two decades. All seven floodgates were opened. The resulting high waters in Sandy Creek closed the Cunningham Highway. The following day SunWater reduced the release rate after requests by Warwick&#39;s mayor.</p><br>
<h2>Fishing</h2><br>
<p>A Stocked Impoundment Permit is required to fish in the dam.</p><br>
<p>Robert F. Kennedy Department of Justice Building is the Washington, D.C., headquarters of the United States Department of Justice.</p><br>
<p>The building is located at 950 Pennsylvania Avenue NW, on a trapezoidal lot on the block bounded by Pennsylvania Avenue to the north, Constitution Avenue to the south, 9th Street to the east, and 10th Street NW to the west, in the Federal Triangle. It is located west of the National Archives Building, east of the Internal Revenue Service Building, north of the National Mall, and south of the J. Edgar Hoover Building. The building is owned by the General Services Administration. It comprises seven floors and 1,200,000 ft&sup2;. It houses Department of Justice offices, including the office of the United States Attorney General. Completed in 1935, it was renamed after the 64th Attorney General of the United States, Robert F. Kennedy, in 2001.</p><br>
<h2>History</h2><br>
<h3>Construction</h3><br>
<p>The Office of the Attorney General was created by the 1st United States Congress by the Judiciary Act of 1789. In 1792, the Congress made the Attorney General a Cabinet-level post. In 1870, President Ulysses S. Grant signed the bill creating the Department of Justice. Still, there was not yet a permanent home for either the Attorney General or the Justice Department, and each had occupied a succession of temporary spaces in federal government buildings and privately owned office buildings. While plans to provide the Department with its own building were developed as early as 1910, it was not until the late 1920s that significant progress was made toward this goal.</p><br>
<p>In 1908 and in 1928, Congress authorized the purchase of land in what is now known as the Federal Triangle for departmental offices. The authorization was part of a wave of government construction; the 1926 Public Buildings Act permitted the government to hire private architects for the design of federal buildings, which led to large-scale construction of public buildings, including the development of the 70 acre Federal Triangle site between the Capitol and the White House. Treasury Secretary Andrew W. Mellon and the Board of Architectural Consultants, composed of leading architects and headed by Edward H. Bennett of the Chicago architectural firm of Bennett, Parsons & Frost, developed design guidelines for the site. Under Bennett&#39;s direction, each member of the board designed one of the buildings in the Federal Triangle complex to "provide each government agency or bureau with a building that would address its functional needs, while combining the individual buildings into a harmonious, monumental overall design expressive of the dignity and authority of the federal government."</p><br>
<p>Milton Bennett Medary of the Philadelphia firm Zantzinger, Borie & Medary was selected as the architect for the Department of Justice Building; upon Medary&#39;s death in 1929, the project was taken over by his two partners Charles L. Borie, Jr. and Clarence C. Zantzinger.</p><br>
<p>In 1930, Congress appropriated $10 million for the construction of a permanent Department of Justice headquarters in the Federal Triangle. The building was constructed from 1931 to 1934. Upon completion in 1935, the building finally provided a headquarters for the Attorney General and Department of Justice. From 1935 to 1941 68 murals were painted in the building (an example of New Deal art).</p><br>
<h3>Post-construction</h3><br>
<p>In 1966, the Department of Justice building was listed on the National Register of Historic Places as part of the Pennsylvania Avenue National Historic Site.</p><br>
<p>In 1974, the Federal Bureau of Investigation, which had been headquartered in the same building, moved into its own headquarters at the J. Edgar Hoover Building across the street on Pennsylvania Avenue.</p><br>
<p>In 1978, the United States Foreign Intelligence Surveillance Court (FISC) was established after the passage of the Foreign Intelligence Surveillance Act. The court of 11 judges appointed by the Chief Justice of the United States (increased from seven by the USA PATRIOT Act) meets in secret "behind a cipher-locked door in a windowless, bug-proof, vault-like room guarded 24 hours a day on the top floor of the Justice Department building," which columnist James Bamford likened to "a modern Star Chamber."</p><br>
<h3>Renovations</h3><br>
<p>From March 1998 to January 2006, major renovations to the building took place, including work on plumbing, electrical wiring, heating and cooling, and elevators. The project included replication of original lighting for the building&#39;s corridors and other ornamental spaces. A new $3.1 million conference center and "data room" were built, the main library and executive suites were restored, and a new mechanical, electrical and plumbing (MEP) system was installed.</p><br>
<p>The project&#39;s submitting firm and construction manager was the Gilbane Building Company, the architectural firm was Burt Hill Kosar Rittelmann Associates, the structural engineering firm was Delon Hampton Associates, and the mechanical/electrical engineer was H.F. Lenz Company.</p><br>
<p>Several difficulties were present: The building had to remain operational during renovations, and hazardous materials were involved, with a large-scale asbestos abatement effort, lead paint removal, and the handling of mercury-vapor lamps with PCBs. The Gilbane Building Company established a "stop-work" rule to halt construction when hazardous material was discovered. An additional complication was security concerns, because of sensitive and classified information in the building. According to Building Design & Construction, construction personnel were "classified into three tiers and were permitted access to specific building areas based on these three levels of security clearance." The extensive murals, sculptures, and plaster reliefs in the building were protected with shields during the construction, and temperature, humidity, and dust controls were installed.</p><br>
<p>The cost of the renovations was $142 million, but the project came in $4.2 million under budget, in part due to significant conservation efforts. Design consultants decided to renovate courtyard plaza and garage structures instead of demolishing them, using 95 percent of existing materials. Cobblestone blocks in the courtyard were "removed, cleaned, refurbished, and reinstalled," with "the foundation of the courtyards original fountain" being preserved and its pipes and pumps replaced. Further, only the concrete of "questionable integrity around the facilitys garage beams" was repaired, instead of having all the concrete replaced. For the plaza deck, the integrity of the concrete structure was tested. Some sections were found to be repairable, preventing them from being rebuilt and diverting 14,520 tons of waste from landfill. Finally, the original foundation and structure building was preserved, which saved 110 tons of waste material and decreased "the risk of penetrating a sensitive waterproofing membrane system." Additional costs were saved through "early buyout": "taking advantage of the purchasing power of the entire four-phase construction job," the construction management firm "was able to secure prices early on in the project that otherwise would have been spent covering the escalating costs of building materials."</p><br>
<p>These measures allowed the GSA to carry out additional work: "restoration and repointing of the limestone exterior," repair and replacement of the roof, restoration of "ornate painting and plaster," further hazardous materials abatement, and fire code upgrades. Ultimately close to $1 million was returned to the GSA.</p><br>
<h3>Renaming</h3><br>
<p>In 2001, the Department of Justice Main Building was renamed the Robert F. Kennedy Department of Justice Building in honor of Robert F. Kennedy, who was Attorney General (1961–1964) under his brother, President John F. Kennedy, and his successor, President Lyndon Johnson. Kennedy was later a USA Senator from New York and presidential candidate until his assassination in 1968. and gave the rededication address on November 20, 2001. Attorney General John Ashcroft also rededicated it in a speech at the Justice Department.</p><br>
<p>Today the building retains exceptional historic integrity. The original facades, lobbies, corridors, library, Great Hall, executive suites and private offices retain their original materials and design, including the extensive use of ornamental aluminum.</p><br>
<p>The building has been the site of demonstrations on the streets outside. On November 16, 2007, African American leaders led by Al Sharpton, Martin Luther King III, and Charles Kenzie Steele, Jr. protested in a march on Pennsylvania Avenue to the Justice Department against perceived racial inequality in the justice system. The protest was precipitated by the case of the Jena Six.</p><br>
<h2>Design</h2><br>
<p>The inscription on one of the sides of the Robert F. Kennedy Department of Justice Building is, "Justice is founded in the rights bestowed by nature upon man. Liberty is maintained in security of justice."</p><br>
<p>It is distinguished from other Federal Triangle buildings by Art Deco elements and the innovative use of aluminum for details that were traditionally cast in bronze. All entrances to the building feature 20 ft-high aluminum doors that slide into recessed pockets. Interior stair railings, grillwork, and door trim are aluminum, as are Art Deco torchieres, doors for the building&#39;s 25 elevators, and more than 10,000 light fixtures.</p><br>
<p>The building has many distinctive interior spaces, including the Great Hall entry foyer and the Law Library. The two-story Great Hall features Art Deco light fixtures and a terra-cotta tile floor with gray marble borders. The Law Library, located on the fifth floor, is a two-story room distinguished by a pair of tall Art Deco lights and a 20-panel mural by Maurice Sterne.</p><br>
<h2>Art</h2><br>
<p>The building contains the largest historic art collection of any General Services Administration–built facility. Sculpture is integrated into the fabric of the building. Sculptors C. Paul Jennewein and Warren Straton were selected to create a unified design concept for the building&#39;s exterior and interior spaces, designing 57 sculptural elements for the building. Their work ranged from the carved limestone figures for the pediments on the Constitution Avenue facade, to the aluminum Art Deco torchieres and light fixtures throughout the interior.</p><br>
<p>The interior of the USA Department of Justice building contains many decorative wall paintings. The building&#39;s extensive murals depict scenes of daily life from throughout American history and symbolic interpretations or allegories relating to the role of justice in American society. In all, 68 murals were completed between 1935 and 1941, at a cost of $68,000, one percent of the cost of the building. Mural artists include George Biddle, Henry Varnum Poor, John Steuart Curry, Boardman Robinson, and Leon Kroll.</p><br>
<p>The striking, colorful concrete mosaics on the ceilings of the vehicular and pedestrian entryways from 9th and 10th Streets were created by the Washington, D.C. master craftsman John Joseph Earley, an innovator in the aesthetic applications of the material. Visible from the street, these mosaics retain much of the brilliance of their original colors.</p><br>
<p>A sculpture of the Revolutionary War hero Nathan Hale by Bela Pratt stands on the southern side of the building.</p><br>
<h3>Spirit of Justice</h3><br>
<p>Spirit of Justice is a cast aluminum Art Deco statue designed by Jennewein. It depicts Lady Justice (a woman wearing a toga-like dress with one breast revealed and arms raised) and stands on display along with its male counterpart Majesty of Law in the Great Hall. Unlike many representations of Lady Justice, Spirit of Justice wears no blindfold to symbolize blind justice. The statue measures 12.5 feet (150 inches) and was commissioned in 1933 at a cost of $7000, and has stood with Majesty of Law in the Great Hall since 1936.</p><br>
<p>In 1986, the statue was seen behind then–Attorney General Edwin Meese during a press conference as he discussed the final report of the Attorney General&#39;s Commission on Pornography (Meese Report). According to the Associated Press, "photographers dived to the floor to capture the image of him raising the report in the air, with the partially nude female statue behind him".</p><br>
<p>In 2002, under Attorney General John Ashcroft, curtains were famously put up blocking the bare-breasted statue from view during speeches. Later, however, internal e-mails surface referred to "hiding the statues" and "the episode was quickly seized upon by pundits and satirists as a symbol of Ashcrofts allegedly puritanical and censorious bearing." Journalist and writer Claire Braz-Valentine wrote an open lyrical letter to Ashcroft, which included the lines "John, John, John,/youve got your priorities all wrong."</p><br>
<p>Ashcroft joked about the incident on the Late Show with David Letterman in April 2002.</p><br>
<p>The curtains were removed on June 24, 2005, under Ashcrofts successor Alberto Gonzales. Justice Department spokesman Kevin Madden was quoted as saying that "the decision to remove the drapes was made by Paul Corts, assistant attorney general for administration, and that Attorney General Alberto R. Gonzales agreed with the recommendation."</p><br>
<p>The Church of the Epiphany, built in 1844,Washington City August 15, 1843 The Sun ; Aug 16, 1843; ProQuest Historical Newspapers The Baltimore Sun </p><br>
<p>pg. 4 is an historic Episcopal church located at 1317 G Street, N.W., in Washington, D.C. It was added to the National Register of Historic Places on September 10, 1971.</p><br>
<p>The parish had been organized in 1842, and the new building consecrated in 1852. During the next five years, a tower, transepts and chancel were added. In 1858, the congregation established the Epiphany Church home to help the poor and sick. The American Civil War split the congregation. As Senator, Jefferson Davis had rented pew no. 14, and three of his children were confirmed at the church. After secession, when Davis moved to Richmond, Virginia and became the Confederacy&#39;s President, that pew was rented by Secretary of War Edwin Stanton. On March 6, 1862, President Abraham Lincoln attended the funeral of General Frederick Lander at this church, which also served as a hospital between May and December of that year.</p><br>
<h2>National Register listing</h2><br>
<p>Church of the Epiphany ** (added 1971 - Building - #71000996)</p><br>
<p>1317 G St., NW., Washington</p><br>
<p>Historic Significance: Event, Architecture/Engineering</p><br>
<p>Architect, builder, or engineer: Harkness, John W.</p><br>
<p>Architectural Style: Gothic Revival</p><br>
<p>Area of Significance: Religion, Architecture</p><br>
<p>Period of Significance: 1825-1849, 1850–1874</p><br>
<p>Owner: Private</p><br>
<p>Historic Function: Religion</p><br>
<p>Historic Sub-function: Religious Structure</p><br>
<p>Current Function: Religion</p><br>
<p>Current Sub-function: Religious Structure</p><br>
<p>Mount Rose is the highest mountain in Washoe County, within the Carson Range of Nevada, United States. It ranks thirty-seventh among the most topographically prominent peaks in the state. It is also both the highest and most topographically prominent peak of the greater Sierra Nevada range within the state of Nevada, and the third most topographically prominent peak in the Sierra Nevada overall. It is located in the Mount Rose Wilderness of the Humboldt-Toiyabe National Forest. An extinct volcano, the mountain is in between Lake Tahoe and Reno.</p><br>
<p>State Route 431 traverses Mount Rose Summit southeast of Mount Rose. Due to the high elevation, most of the precipitation that falls on the mountain is snow.</p><br>
<p>The view from Mount Rose, facing east is the Truckee Meadows area is the second largest population center in Nevada.</p><br>
<p>Mount Rose Ski Tahoe is nearby but is not on Mount Rose. Despite the name, the resort is actually on the slopes of Slide Mountain, which is on the other side of Nevada State Route 431. The east slope of Slide Mountain, is the East Bowl of Mt. Rose. In 1964, the north side of Slide Mountain was named Mount Rose Ski Area and Reno Ski Bowl was renamed Slide Mountain Ski Area. In 1987 the two ski areas merged and began operation as one resort named Mt. Rose.</p><br>
<p>Dr. James Edward Church of the University of Nevada established the Mount Rose Weather Observatory, one of America&#39;s first high-altitude meteorological observatories, on June 29, 1905.</p><br>
<h2>Summit panorama</h2><br>
<h2>Climate</h2><br>
<p>John Brayshaw Kaye, a poet, lawyer and politician, wrote a poem called Mount Rose</p><br>
<p>Florence Peak is a mountain located on the Great Western Divide, a sub-range of the southern Sierra Nevada of California. It is located about 6 mi southeast of the community of Silver City and 4.5 mi from the roads end at Mineral King. It marks the southern boundary of Sequoia National Park. On the summit the Sequoia-Kings Canyon Wilderness, the John Krebs Wilderness and Golden Trout Wilderness meet.</p><br>
<h2>Geography</h2><br>
<p>The peak rises to an elevation of 12,438 ft, making it one of the highest mountains south of Mount Whitney. The Franklin Lakes, a series of tarns, lie in a cirque on north side of the peak and these drain into the Kaweah River by way of Franklin Creek. The eastern slopes drain into the Kern River. The southwestern flank drains into the 10,000 ft Bullfrog Lakes and thence into the Little Kern River.</p><br>
<p>The high elevation of the peak means that most of the precipitation it receives falls as snow.</p><br>
<p>The Fred Haigh Dam  was constructed across the Kolan River in 1978 creating Lake Monduran. The dam&#39;s catchment area, north of Bundaberg in Queensland, covers 1310 square kilometers.</p><br>
<h2>Spillway Upgrade</h2><br>
<p>SunWater is undertaking a dam spillway capacity upgrade program to ensure the highest level of safety for the dam is maintained. The spillway will be upgraded before 2010.</p><br>
<h2>Boating</h2><br>
<p>There are no boating restrictions on the lake and there is a single boat ramp for boat access.</p><br>
<h2>Fishing</h2><br>
<p>The dam has been stocked with barramundi, silver perch, sooty grunter and red-claw crayfish with spangled perch and forktail catfish naturally present. A Stocked Impoundment Permit is required to fish in the dam.</p><br>
<p>Construction of Bjelke-Petersen Dam near Cherbourg in Queensland, commenced in 1984 and finished in 1988. It created the lake that was named Lake Barambah after the original property in the region. The dam supplies water to the South Burnett region, mostly for irrigation purposes.</p><br>
<p>The dam wall is 540 m long and rises 34 m. The wall is an earth and rock fill structure with a central clay core, which can hold back 134,900 ML of water. The dam is generally shallow. Barker Creek provides the main inflow, while Four Mile Creek, Six Mile Creek, Frickey Creek and Cattle Creek also flow into the dam.</p><br>
<h2>History</h2><br>
<p>In the 1990s management of the camping and recreational facilities was handed to Murgon Shire Council. Facilities for caravans, cabins, camping and day-trippers are extensive. Under normal conditions there are no boating restrictions, except near the dam wall.</p><br>
<p>In 2006, drought conditions had reduced dam levels to 5% of total capacity. With such low levels, visitors numbers had dropped significantly and local councils were concerned about maintaining drinking water for local towns.</p><br>
<p>SunWater, the managing organisation of the dam, is undertaking a dam spillway capacity upgrade program to ensure the highest level of safety for their dams is maintained. The spillway upgrade commenced in 2007.</p><br>
<h2>Fishing</h2><br>
<p>The dam is stocked with bass, golden perch, silver perch and southern saratoga. Additionally eel-tailed catfish, spangled perch and bony bream are present naturally. A Stocked Impoundment Permit is required to fish in the dam. The Bjelke-Petersen Dam Fishing Classic is held every October.</p><br>
<p>Illegally introduced sleepy cod and red-claw crayfish are maintaining breeding populations. In 2002, Tilapia were posing a threat to the dam, resulting in the need for pipeline screening to be implemented in an effort to stop eggs and larvae entering the dam.</p><br>
<p>Boondooma Dam is a dam on the Boyne River on the boundary of Boondooma and Okeden in the South Burnett Region of Queensland, Australia. In 1983, the dam was constructed across the Boyne River below its confluence with the Stuart River.</p><br>
<p>It has a capacity of 204 200 ML under the 10 km&sup2; of surface area and has an average depth of 11 m. The dam forms a narrow and deep lake, designed to avoid evaporation, with one fork containing lots of standing timber and another having many submerged rocky outcrops.</p><br>
<h2>Water supply</h2><br>
<p>It was built to supply water to the Tarong Power Station and as is the case at so many impoundments, takes its name from the original property in the area. The dam also supplies water to irrigate agricultural properties in the area.</p><br>
<p>Typically, the dam supplies between 50 million and 80 million litres of water per day to Tarong Power Station. The dam was connected to the Western Corridor Recycled Water Project to ensure water levels would not interfere with power generation in times of drought.</p><br>
<p>SunWater, the dam&#39;s managing authority, is undertaking a dam spillway capacity upgrade program to ensure the highest level of safety for dams under their jurisdiction is maintained. The spillway will be upgraded in the longer term.</p><br>
<h2>Recreation</h2><br>
<p>Since March 2001, camping and recreational facilities at the dam have been managed by the Wondai Shire Council, and since council amalgamations, South Burnett Regional Council. Self-contained cabins, caravan sites and camping are all available by the lake. There are also multiple picnic grounds for day-trippers. Angling, swimming, sailing and water skiing are all popular activities at Boondooma Dam.</p><br>
<h3>Fishing</h3><br>
<p>The dam is stocked with bass, golden perch, silver perch and barramundi, while eel-tailed catfish, and bony bream are present naturally. A Stocked Impoundment Permit is required to fish in the dam. In 1993 and 1994, more than 60 000 barramundi were released into the dam, thought the furthest south that the species could survive. Limited numbers have been caught since, but greater success was achieved at locations closer to the coast of similar latitude.</p><br>
<h3>Boating</h3><br>
<p>The dam has two boat ramps and a boating permit is not required. There are no boating restrictions on the dam, however a no fishing/boating zone applies around the dam wall.</p><br>
<p>Second Church of Christ, Scientist is a historic former Christian Science church building located at 948 West Adams Boulevard, in the West Adams district of Los Angeles, California. It is now the Art of Living Center Los Angeles.</p><br>
<h2>History</h2><br>
<p>Designed by noted Los Angeles architect Alfred H. Rosenheim in the Classical Revival style of architecture, it was built in 1910.</p><br>
<p>On July 17, 1968, the City of Los Angeles designated the building a Los Angeles Historic-Cultural Monument.</p><br>
<p>The church was used as the courthouse in the crime drama Matlock and as a location for other film and TV projects.</p><br>
<h2>The Art of Living Foundation</h2><br>
<p>In late 2009, the Church property was sold to the non-profit Art of Living Foundation. It was restored and is used as a community center, speaking and music venue, and is a center for the Foundation&#39;s service work and breathing, meditation, and other programs. While the Art of Living Foundation has been active in Southern California since the late 1980s, it officially opened in this location on April 14, 2010.</p><br>
<h2>National register listing</h2><br>
<p>Second Church of Christ, Scientist (added 1987 - Building - #87000576)</p><br>
<p>946 W. Adams Blvd., Los Angeles</p><br>
<p>Historic Significance: Event, Architecture/Engineering</p><br>
<p>Architect, builder, or engineer: Albert C. Martin, Sr., Alfred Rosenheim</p><br>
<p>Architectural Style: Classical Revival</p><br>
<p>Area of Significance: Architecture, Religion</p><br>
<p>Period of Significance: 1900-1924</p><br>
<p>Owner: Private</p><br>
<p>Historic Function: Religion</p><br>
<p>Historic Sub-function: Religious Structure</p><br>
<p>Current Function: Non-profit educational and humanitarian</p><br>
<p>Current Sub-function: Community service, personal development, trauma relief—501(c)(3)</p><br>
<p>Belaya Zemlya  is a group of three cold, glaciated islands. It is a geographical subgroup of Franz Josef Land, Russian Federation.</p><br>
<h2>History</h2><br>
<p>This area was named Hvidtenland (Norwegian: "White Land") by Fridtjof Nansen, who reached this desolate place on August 5, 1895 during his polar expedition. In his map he drew four islands. Since the limit of permanent ice crosses Belaya Zemlya, it is often difficult to distinguish between land and sea. However, as the cartography of the Franz Josef Archipelago became more accurate, it became apparent that it was a group of three islands.</p><br>
<p>Belaya Zemlya is the point of the Franz Josef Archipelago that Valerian Albanov was trying to reach when he left the Svyataya Anna with part of the crew, but owing to the polar ice drift and the abundance of polynias along his route, he ended up far to the southwest in Alexandra Land.</p><br>
<h2>Geography</h2><br>
<p>Belaya Zemlya is separated from the main Franz Josef group by a 45 km broad strait known as Proliv Severo Vostochnyy.</p><br>
<h3>Islands</h3><br>
<p>Eva Island (Остров Ева-Лив), or "Eva-Liv Island", as it includes the Liv Peninsula. With 25 km in length, this is the largest island of the group. Eva Island was named after Fridtjof&#39;s wife Eva Nansen (died in 1907). The island is completely covered by two ice domes.</p><br>
<p>Adelaide Island (Остров Аделаиды). Only 2 km in length, this is a very small island. It is located 5 km to the southwest of Eva Island&#39;s western end. Adelaide Island was named in honor of Princess Adelheid of Hohenlohe-Langenburg.</p><br>
<p>Frieden Island (Остров Фреден), sometimes also spelt "Fryeden" because of the transliteration from the Russian. This is a larger oval-shaped island, with a length of 8.2 km. It lies 2.5 km south of Adelaide Island. Frieden Island is named after the German word for "Peace".</p><br>
<p>Nohkalikai Falls is the tallest plunge waterfall in India. Its height is 1115 feet , making it as the highest waterfall in India. The waterfall is located near Cherrapunji, one of the wettest places on Earth. Nohkalikai Falls are fed by the rainwater collected on the summit of comparatively small plateau and decrease in power during the dry season in December - February. Below the falls there has formed a plunge pool with unusual green colored water.</p><br>
<p>Jeff Jefferson and Steven Stevenson.</p><br>
<h2>The legend of Nohkalikai</h2><br>
<p>According to legends, in a village called Rangjyrteh, upstream from Nohkalikai Falls, a woman named Likai resided but had to remarry after her husband died. Ka Likai (Ka is the prefix given for the female gender in Khasi) was left with her infant girl with no means of income. So she had to become a porter herself. Her work required her to leave her daughter unattended for long intervals but when she would be at home she would spend most of her time taking care of her infant. Ka Likai, who married a second time, couldn’t pay attention to her second husband. The jealous husband killed the infant and cooked her meat after throwing away her head and bones. When Ka Likai returned home, she saw nobody in the house but except for a meal that had been prepared. She wanted to go look for her daughter but she ate the meat as she was tired from work.</p><br>
<p>Ka Likai usually had a betel leaf after her meals but she found a severed finger near the place where she usually cut betel nuts and betel leaves. Ka Likai realized what had happened in her absence and went mad with anger and grief and started running as she swung a hatchet in her hand. She ran off the edge of the plateau and the waterfall where she jumped from was named Nohkalikai Falls after her.</p><br>
<p>Sandy Islands is a small group of four islands located in the northern basin on Lake Winnipeg in the Canadian province of Manitoba. The Sandy Islands together with Little George Island, George Island and the Spider Islands form a chain of islands, which are a continuation of The Pas Moraine.</p><br>
<p>The largest island within the group is Big Sandy Island, located approximately 47 km west from the mouth of the Poplar River on the eastern shore, and approximately 32 km east from the easternmost tip of the Long Point on the western shore of Lake Winnipeg.</p><br>
<p>Other islands in the group are Little Sandy Island to northwest of the main island, and Cannibal Island to southeast. The smallest island is located in the narrow strait between Little Sandy and Big Sandy islands.</p><br>
<p>The islands are uninhabited with no man-made structures present.</p><br>
<p>Clark Mountain is a mountain located in the Clark Mountain Range in the Mojave National Preserve, close to the California-Nevada border.</p><br>
<h2>Geography</h2><br>
<p>The mountain rises abruptly north of Mountain Pass and Interstate 15 to an elevation of 7,933 ft, which is the highest point of the Mojave National Preserve and the Mojave Desert ranges.</p><br>
<p>Path 46 and Path 64 (part of Path 46) 500 kV power lines run to the north and south of the mountain, respectively.</p><br>
<h2>Ecology</h2><br>
<p>The higher elevations of the mountain are a striking sky island contrast to the lower elevations of the Mojave Desert vegetation. Creosote bush (Larrea tridentata), scrub and Joshua tree (Yucca brevifolia) forests grow on the foothills of the mountain while Single-leaf Pinyon Pine (Pinus monophylla), Utah juniper (Juniperus osteosperma), and White fir (Abies concolor) grow on the sky island at the highest elevations.</p><br>
<p>The high elevation of the mountain means that snow falls on the high peaks during the winter, although the mountain receives little precipitation annually.</p><br>
<h2>Recreation</h2><br>
<p>Clark Mountain is also a world-class rock climbing area developed by Randy Leavitt in 1992. It has been described as containing the best limestone climbing in America.</p><br>
<p>The Immaculate Conception Church and School are located at 2708 South 24th Street in the South Omaha area of Omaha, Nebraska, United States. The 1926 church and its former school building, built in 1912, were added to the National Register of Historic Places in 1998. Both buildings were designed by Omaha architect Jacob M. Nachtigall.</p><br>
<h2>Church history</h2><br>
<p>Immaculate Conception Parish is part of the Archdiocese of Omaha. The parish was founded in 1898 and incorporated in 1900. Traditionally the home congregation for many Polish Catholics in Omaha, the present church was built in 1926 and dedicated on July 31, 1927. In August, 2007, Archbishop Elden Curtiss entrusted the care of the parish to the Priestly Fraternity of St. Peter to provide the Mass and sacraments in the traditional rites of the Catholic Church to any who so desired them. The first Traditional Latin Mass in over 40 years was offered on Sunday, August 26, 2007. A personal parish dedicated to the Traditional Latin Mass is encouraged by Pope Benedict XVI in his 2007 Motu Proprio Summorum Pontificum on the Latin Mass.</p><br>
<h2>Other buildings on the property</h2><br>
<p>Immaculate Conception School is located next door at 2716 South 24th Street in South Omaha, Nebraska. The school was sold by the church to private property management firm Guardian Real Estate in the mid-1990s and is now a low-income apartment building.</p><br>
<p>Still owned by the parish is the I.C.C. Recreation Center, built in 1954 and located west of the Church. The center houses a wood-floor gymnasium with stage and kitchen (serving as the parish hall), a rentable party room and the I.C.C. Bowlatorium, one of the last church-owned and operated bowling alleys left in the USA The Bowlatorium is open for leagues, open bowling and party rentals.</p><br>
<p>GoggleWorks Center for the Arts is a community art and cultural resource center located in Reading, Pennsylvania. The mission of the GoggleWorks is “to nurture the arts, foster creativity, promote education and enrich the community.”</p><br>
<p>Located in the former Willson Goggle Factory building, GoggleWorks Center for the Arts features six teaching studios in ceramics, hot and warm glass, metalsmithing, photography, and woodworking; 35 juried artist studios; and dozens of dance, music, and other creative businesses and cultural organizations. GoggleWorks also includes several exhibition galleries, a 130-seat film theatre, cafe, and gift store featuring handcrafted works by over 200 artists working within the building and beyond. Admission (excluding special events) and parking are always free.</p><br>
<p>The building was added to the National Register of Historic Places in 2006.</p><br>
<h2>History of the GoggleWorks Building</h2><br>
<p>Founded by Gile J. Willson and his son Dr. Thomas A. Willson in 1871, Thomas A. Willson & Co. opened the first factory in the world to manufacture optical glass for lenses and reading glasses. Located at the corner of Washington and 2nd streets in Reading, Pennsylvania, the company became known for its innovative strides in addressing the occupational hazards faced by factory workers and is credited with launching the safety protection industry. Their first innovation was a protective lens that blocked dangerous and blinding rays produced by metal processing equipment. During the 1890s the company expanded the reach of the safety industry addressing hearing, respiratory and head protection equipment.</p><br>
<p>The National Safety Council was created in 1913, and T.A. Willson & Co. Inc. Helped to set the uniform safety standards in industry. Through the 1920s, they expanded their line of safety equipment to the protection of coal miners, military personnel, and aviation. In 1929 the company became Willson Goggles, Inc., and by World War II, Willson Goggles was helping the war effort by making aviator goggles and high altitude oxygen masks for pilots in the military. In 1936, the company again changed its name to reflect an expanding product line. Willson Products, Inc. began to produce fashionable sunglasses, as modeled by the contestants of the 1938 Miss America pageant, and swim goggles, as worn by Florence Chadwick, who in 1950 was the first woman to swim both directions of the English Channel.</p><br>
<p>The company changed hands in 1956, but maintained the Willson products name through the atomic age and space age, still leading the safety industry in research and development of equipment to meet the needs of a technologically advancing society.</p><br>
<p>In the 1980s, Willson shifted its focus to the development of new varieties of respirators, gloves and other protective equipment. In 1989, Dalloz bought Willson products, and changed the company name to Dalloz Safety in 1997. Dalloz closed the plant in May 2002.</p><br>
<h2>Recent Developments and Uses</h2><br>
<p>In 2005, the concept of the GoggleWorks came to fruition when Albert Boscov and Marlin Miller took over the building. It opened its doors on September 18, 2005. In the October/November 2006 issue, American Crafts comments:</p><br>
<p>"Combining Boscov’s flair for promotion (he was chairman of the Boscov’s department store chain) with Miller’s longtime involvement in the craft world as a collector and advocate (he’s currently board chair of the Haystack Mountain School of Crafts), they envisioned a broad-based arts center built around artists’ studios… he city got behind the idea, as did the state, which gave three million dollars in initial funding."</p><br>
<p>Since then, a capital campaign and volunteers, along with the artists, staff, and board members, have helped to keep the GoggleWorks a working success.</p><br>
<p>Grand Lake is a 5,660 acre lake in Presque Isle County in the USA state of Michigan. Grand Lake is a substantial lake of approximately 7 miles  in length and up to 1.5 miles  in width. The lake is on the boundary between Presque Isle Township to the east and Krakow Township to the west, approximately 15 miles  north of Alpena on USA Highway 23, which passes to the south and west of the lake.</p><br>
<p>Fishing species include: bluegill, bullhead catfish, northern pike, garpike, bowfin, pumpkinseed sunfish, rock bass, smallmouth bass, white sucker, yellow perch, and walleye.</p><br>
<p>The lake lies on the landward side of a prominent promontory in the county that juts out into Lake Huron, thereby making the promontory almost an island and indirectly giving the promontory and county their name of "Presque Isle." The lake contains many islands, such as Brown Island, Grand Island, and Macombers Island.</p><br>
<p>The two Presque Isle, Michigan lighthouses are nearby to the east: the New Presque Isle Lighthouse at 4500 E. Grand Lake Road and the Old Presque Isle Lighthouse at 5295 Grand Lake Road.</p><br>
<p>Deposits of Rock salt were discovered at a depth of 1284 feet in the vicinity of Grand Lake. On the west shore of the lake are ledges, which rise to a height of 40 feet above lake level, and include Cerepatora fossils along with crinoid stems.</p><br>
<p>Gordonbrook Dam is a dam in Gordonbook, South Burnett Region, Queensland, Australia. It is the main source of water supply for Kingaroy in the Wide Bay-Burnett area. It was built in 1941 to provide water for the Royal Australian Air Force Training Base during World War II. In 1987, due to increased demand, the dam wall was raised, and the inundated area is now 229 hectares.</p><br>
<h2>Recreation</h2><br>
<h3>Land</h3><br>
<p>A basic picnic area is located on the eastern shores. The picnic area is fairly large and contains a composting toilet, a water tank, picnic tables, a boat ramp, information signs and a bush walk that includes an elevated lookout and a well maintained bird hide.</p><br>
<h3>Water</h3><br>
<p>When the lake area is open to public recreation, the dam provides a good range of water-based activities. The lake is largely accessible to small to medium-sized motorised boats, jetskis, canoes and windcraft. The body provides the best space for water skiing and water tubing, while the foot is best suited for boat fishing and non-motorised craft only, because of the large stands of dead timber.</p><br>
<h3>Fishing</h3><br>
<p>A Stocked Impoundment Permit is required to fish in all parts of the dam.</p><br>
<h2>Blue green algae infestation</h2><br>
<p>During dry periods and because the dams smaller size, the dam experiences high levels of blue green algae (Cyanobacteria). Activities are at the users own risk, and the boat ramp has gates to prevent motorised craft from entering the water during times of high risk of the algae.</p><br>
<p>Chauncey Peak, 688 ft, is a traprock mountain located 2 miles  northeast of the center of Meriden, Connecticut. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border. Chauncey Peak is known for its scenic vistas, vertical cliff faces overlooking Crescent Lake, unique microclimate ecosystems, and rare plant communities. It rises steeply 400 ft above the city of Meriden to the south with west-facing cliffs that plunge into Crescent Lake 300 ft below.</p><br>
<p>The mountain is traversed by the 50 mi Mattabesett Trail.</p><br>
<h2>Geography</h2><br>
<p>Roughly 0.75 miles (1.2 km) in diameter, Chauncey Peak is located within the town of Meriden, Connecticut. Although Chauncey Peak is described by some sources as part of Lamentation Mountain, PDF brochure. South Central Regional Council of Governments. North Haven, Connecticut. Undated. Cited December 17, 2007.</p><br>
<p>it rises more than 300 ft above the common gap between the two, making it its own mountain by regional standards (see Four-thousand footers). Crescent Lake, (formerly called Bradley Hubbard Reservoir), lies nestled between Lamentation Mountain and Chauncey Peak. The lake provides emergency drinking water to the city of Meriden. Much of the east side of the mountain has been subject to quarrying; as of 2007, the quarry was.5 mi (.8 km) wide, roughly 3/4 the width of the entire mountain. Interstate 91 cuts through the gap between Higby Mountain and Chauncey Peak to the north.</p><br>
<p>The Metacomet Ridge continues north from Chauncey Peak to become Lamentation Mountain and south to become Higby Mountain. The western half of Chauncey Peak drains into the Quinnipiac River, then to Long Island Sound; the eastern half to the Mattabesett River, thence to the Connecticut River and Long Island Sound.</p><br>
<h2>Geology and environment</h2><br>
<p>The origin of Chauncey Peak and the Metacomet Ridge dates back 200 million years ago with the rifting apart of North America from Eurasia in the process that would ultimately create the Atlantic Ocean. In the area that is now the Metacomet Ridge and surrounding sedimentary rock basin, massive basalt (traprock) lava flows spread across the prehistoric rift valley, some of them several hundred feet thick, over a period of 20 million years. Sediment accumulated between lava flows and lithified into sedimentary rock. After the rifting processes ceased, layers of strata faulted and tilted upward. Subsequent erosion, glaciation, and uplift exposed the weather resistant edge of the traprock lava sheets, creating the cliffline of the Metacomet Ridge as it is today. The mineral content and the shape of the ridge make possible a variety of microclimate ecosystems. Hot and dry cliff faces support plant and animal species uncommon so far north. Deeply gouged ravines support cooler climate species found in more northerly climes, while gradual backslope environments support species typical of the surrounding latitude. Talus slopes beneath cliffs accumulate minerals that support alkaline-loving plant species uncommon in surrounding acidic southern New England. Extensive cliffs provide ideal habitat and important migration corridors for raptor species.</p><br>
<h2>Recreation and conservation</h2><br>
<p>The west side of Chauncey Peak lies within Giuffrida Park, managed by the city of Meriden. The park boasts a lake, golf course, woodlands, and the rocky peaks of Lamentation Mountain and Chauncey Peak. Permitted activities within the park include hiking, snowshoeing, cross-country skiing, picnicking, and bicycling. Swimming, boating, rock climbing, and fishing are prohibited. The park supports a number of trails, most notably the Mattabesett Trail (maintained by the Connecticut Forest and Park Association), which stretches from the northern end of Lamentation Mountain, south to Totoket Mountain and north again to the Connecticut River. Trailhead parking for Chauncey Peak is located at Giufridda Park on Westfield Road, 1.2 mi east of its junction with USA Route 5 and 1.8 mi west of Interstate 91, exit 20, via Country Club Road (which becomes Westfield Road).</p><br>
<p>The ecosystem and ridgeline of Chauncey Peak is most threatened by quarrying, although the west side of the peak, within Giuffrida Park, is protected. In 2000, Chauncey Peak was included in a study by the National Park Service for the designation of a new National Scenic Trail now tentatively called the New England National Scenic Trail, which would include the Metacomet-Monadnock Trail in Massachusetts and the Mattabesett Trail and Metacomet Trail trails in Connecticut.</p><br>
