<p>First Presbyterian Church, also known as First United Presbyterian Church, Templar Lodge No. 514, and the West Bend Historical Museum, is a historic building located in West Bend, Iowa, United States. The first recorded Protestant services in town were led by a Presbyterian minister, the Rev. David S. McComb in 1851. First Presbyterian Church was chartered on December 23, 1883 with 11 members. The Rev. Harvey S. Dickey served as their first pastor. They initially worshiped in homes until they built this church building in 1889. An addition was constructed onto the rear of the building in 1915 as the congregation grew. They continued to worship here until 1972 when lack of numbers forced them to disolve. Templar Lodge No.514 took over the building at that point and used it until December 14, 1977. The West Bend Historical Society aquired the building and used it for a museum from 1981 until 2007.</p><br>
<p>The building is considered a rare example of a wood-frame Late Victorian church. The exterior suggests a vernacular form created by a local craftsman. It utilizes religious symbolism as decorative elements, such as the triangular hoods on the windows and doors that refer to the Holy Trinity. The narthex on the interior reflects the Victorian period of its construction, while the sanctuary reflects the Classical influences popular when the 1915 addition was constructed. The building was listed on the National Register of Historic Places in 2010.</p><br>
<p>Loucks Grove Church  is a historic church in Greenfield, Iowa.</p><br>
<p>It was built in 1895 and added to the National Register of Historic Places in 1995. Its National Register nomination notes its significance as follows:Loucks Grove Church stands as the lone example of an unchanged Gothic influenced rural religious building of the late 19th century in Adair County, Iowa. Such buildings represented about two-thirds of the county&#39;s churches in 1895. It is a simple, white, frame building that has withstood the test of time and has undergone no structural changes in one hundred years. With the exception of electricity and a propane space heater, it is today as it was then in 1895. The vestibule with its decorative hardware on the doors and an ogee arch window, and the sanctuary with its pointed arch windows and rounded ceiling that exhibit the Gothic influence still show the original design and construction. It is the only church in Adair County with such a distinction.</p><br>
<p>The congregation was a member of the Christian Church from 1895 to 1957, and a non-denominational church after that.</p><br>
<p>Coldwater Church of the Brethren is a historic church building located in Greene, Iowa, United States. The Church of the Brethren congregation was established by Philip Moss in Coldwater Township in 1855. Initially, they held their services in area schoolhouses. The town of Green was established in 1871, and they chose to build their church there in 1873. Philip Moss&#39; son Aaron built the church. It is a 40 by front gable structure built over a raised basement. The stone was quarried locally. It is thought the lower level was used as a parsonage until a frame dwelling was erected to the east of the church in 1915. Originally one room, the upper level has been divided to create two Sunday school rooms at one end. The church building was added to the National Register of Historic Places in 1979.</p><br>
<p>Albright Memorial Building, also known as Scranton Public Library, is a historic library building located at 500 Vine Street in Scranton, Lackawanna County, Pennsylvania. Designed in 1890 and completed in early 1893, it is a two-story, "L"-shaped, Indiana limestone and Medina sandstone building with Châteauesque-style design elements. It consists of a main building measuring 36 feet by 132 feet and a wing set a right angle and measuring 30 feet by 52 feet. It was designed by the noted Buffalo, New York architectural firm of Green & Wicks. The building was donated by Buffalo entrepreneur and philanthropist and former Scranton resident, John J. Albright, who dedicated it in memory of his parents. Albright was also a founder of the Albright–Knox Art Gallery in Buffalo.</p><br>
<p>It was added to the National Register of Historic Places in 1978.</p><br>
<p>The former First Church of Christ, Scientist, also listed on the National Register, now serves as the Children&#39;s Library and is located immediately southeast of the main library.</p><br>
<p>Dime Bank Building, also known as the Dime Bank & Trust Company Building, is a historic commercial building located at Scranton, Lackawanna County, Pennsylvania. It is a five-story brick building in the Richardsonian Romanesque style. The original three-story building was built in 1890-1891, and measured 70 by. Soon after, an additional two-stories were added, as well as a wing measuring 30 by. In 1908, the building was again expanded with a concrete and slab fireproof wing. The facade features a delicately ornamented bay window, five-story turret, and three-story rectangular projection terminated at the third floor by a large arched masonry opening.</p><br>
<p>It was added to the National Register of Historic Places in 1978. It is located in the Lackawanna Avenue Commercial Historic District.</p><br>
<p>The Robert N. C. Nix Sr. Federal Building and United States Post Office, formerly known as the United States Court House and Post Office Building, is a historic building in Philadelphia, Pennsylvania. Built in 1937–1941, it was designed by Harry Sternfeld in the Moderne style and features several sculptures and reliefs by Donald De Lue and Edmond Amateis. It was renamed in December 1985 in honor of Robert N.C. Nix Sr., a longtime Democratic Congressman from Pennsylvania&#39;s 1st Congressional District in Philadelphia, and the first African-American to represent Pennsylvania in Congress.</p><br>
<p>The building was listed on the National Register of Historic Places in 1990.</p><br>
<h2>Architecture</h2><br>
<p>The building is in Center City Philadelphia on a 2 acre lot bounded by Market Street to the north, Ninth Street to the east, and Chestnut Street to the south, and an alley to the west. Its seven stories have a height of about 115 ft above grade and include a basement, a mezzanine between the first and second floors, and two penthouses. It measures 170 ft along Chestnut and Market Streets by 470 ft along Ninth Street. A light court provides access to outside air and light from the third to the sixth floor.</p><br>
<p>The steel structure is encased in concrete and the foundation and basement walls are reinforced concrete. Interior walls are concrete, clay tile, or brick. The base of the building is faced with Milford pink granite with Indiana limestone covering most of the facades facing the street. Buff-colored brick covers the facades of the interior light court.</p><br>
<p>Central air-conditioning was a feature of the original construction, but records indicate that more than 270 window units were installed over time, and then removed during a 1989 restoration. Handicapped access was installed at the eastern entrance on Market Street, but otherwise the exterior appears as it was originally designed.</p><br>
<p>The first floor is occupied by a post office, while courtrooms and a law library occupy the second floor. Upper floors contain offices, open plan office space, meeting rooms and similar spaces. The National Archives at Philadelphia is entered on Chestnut Street. The facility "maintains the historically significant records of the Federal Agencies and Courts, in Delaware, Maryland, Pennsylvania, Virginia and West Virginia, dating from 1789 to the present" and is open to the public.</p><br>
<p>Periya aeri , also known as Pallavaram aeri or Pallavaram lake, is situated on eastern side of railway track from Pallavaram to Chromepet, Chennai, Tamil Nadu. It used to be a large lake but it dried up and was polluted by industrial waste water and garbage.</p><br>
<p>A burial site remains and is used for burial rites.</p><br>
<h2>Ecological impact</h2><br>
<p>This lake was once huge and the railway tracks and trains passing through were visible from the banks of the lake. The lake does not have a single a drop of water and has turned into a dumpyard with huge garbage piles.</p><br>
<p>The lake&#39;s health was altered by the following:</p><br>
<p>Waste waters from Chrome leather companies situated on western side mixes in the lake. The lake has shrunk due to huge encroachment and illegal buildings and constructions that took place over the decade.</p><br>
<p>On the eastern side, portions of the lake&#39;s banks were demolished in order to shell out the water from the lake to pave way for construction of road in 2001.</p><br>
<p>More over the lake was cut in to two by Radial road connecting Chromepet, Pallavaram to Thoraipakkam.</p><br>
<p>There is also a huge encroachment inside the lake on Southwest side. The compound walls of that encroachment runs inside the lake from one end to almost to other end.</p><br>
<p>The Pallavaram Lakes are well encroached by getting the green signal of authorities right from Collector to VAOs.</p><br>
<p>They are directly involved in destroying the lakes and encouraging the Water mafias to make drinking water as commodities.</p><br>
<p>Kanchipuram Collector is the main person behind this along with Pallavaram Municipal commissioner and Councillors.</p><br>
<h2>Burial ground</h2><br>
<p>There is a burial ground situated on south eastern end of the lake (behind Lakshmi nagar and Ganapathy puram). People perform last rites and immerse the ashes in the lake.</p><br>
<p>James Madison School, also known as East Scranton Intermediate School and East Scranton Junior High School, is a historic school building located at Scranton, Lackawanna County, Pennsylvania. It was built in 1927-1928, and is a three-story, "C"-shaped steel frame, brick, and reinforced concrete building in an eclectic Late Gothic Revival / Classical Revival style. It measures approximately 105 feet by 165 feet and has a flat roof. The building has undergone little alteration since it original construction.</p><br>
<p>It was added to the National Register of Historic Places in 2009.</p><br>
<p>In 2015, the building was renovated to house an early childhood learning program as well as apartments for graduate students at the University of Scranton.</p><br>
<p>Roger Williams Public School No. 10, also known as South Scranton Catholic High School, is a historic school building located at Scranton, Lackawanna County, Pennsylvania.</p><br>
<h2>Description</h2><br>
<p>It was built about 1896, and is a two-story, "I"-shaped brick and sandstone building in a Late Victorian style. It features a central three-story entrance tower with a hipped roof. A two-story brick addition was built in 1965.</p><br>
<p>The public school was closed in 1941, and subsequently acquired by the Roman Catholic Diocese of Scranton for use as a consolidated Catholic high school. It was renamed in 1973, as Bishop Klonowski High School, and closed in 1982.</p><br>
<p>The property was acquired by Lackawanna Junior College in 1982. In 2012, it is occupied by Goodwill Industries.</p><br>
<p>It was added to the National Register of Historic Places in 1997.</p><br>
<p>St. John&#39;s Episcopal Church in southeast Portland in the USA state of Oregon is a one-story structure listed on the National Register of Historic Places. Built in 1851, it was added to the register in 1974. It is the oldest intact church building in Oregon. The church is also known as the Oaks Pioneer Church.</p><br>
<p>Located in Oaks Pioneer Park in the Sellwood neighborhood, the rectangular post-and-beam structure has a footprint of 18 by. Fashioned from a partly completed house owned by pioneer Lot Whitcomb, it was the first Episcopal church in Oregon.</p><br>
<p>Whitcomb was a steamboat operator who founded the community of Milwaukie. The church, originally sited on the outskirts of Milwaukie, was moved nearer the towns center in 1862. Modifications over the years included revisions to the chancel in 1869 and the windows, siding, and belfry in 1888. The belfry contains a ships bell that belonged to Whitcomb.</p><br>
<p>Supplanted by a new church building in 1948 (St. John the Evangelist Episcopal Church in Milwaukie, Oregon) and scheduled for demolition in 1969, the church was saved by private interests that paid to float it down the Willamette River on a barge and install it in Oaks Pioneer Park. In the 21st century, the church functions as a museum and wedding site.</p><br>
<p>Skålvær are a group of islands in the municipality of Alstahaug in Nordland county, Norway. The islands are located in the western part of Alstahaug, about 15 km northwest of Tjøtta and about 15 km south of Silvalen . They were formerly a part of Vega, but in 1971 it was transferred to Alstahaug.</p><br>
<p>Skålvær was once a thriving trading post and had many residents, but it has since declined in importance. Today, much of Skålvær is an outdoor recreation area for Alstahaug municipality. In addition, there are about fifteen private houses and cottages scattered around the main island. There are no longer any permanent residents on Skålvær, but the place is far from abandoned. Summer residents live on the island, and Skålvær Church holds services on the island infrequently.</p><br>
<p>Meenuliyan Para or Meenulinjan para  is a mountain peak situated near Thodupuzha in Idukki district, in the Indian state of Kerala. Para in Malayalam language means a rock. Meenuliyan para is noted for a huge rock that rises more than 4000 feet and has about two acres of evergreen forest on top of it. The rock itself covers an area more than 500 acres. The surface of this huge rock mountain looks like fish scales and hence the mountain gets the name ‘ Meenuliyan Para’. The lofty peaks of the Meenuliyan para are covered in mist on rainy days but on a fine day the lower Periyar area, Bhoothathankettu and even Ernakulam are visible from these heights.</p><br>
<p>Meenuliyan para is located 47 km from Muvattupuzha and 51 km from Thodupuzha. Meenuliyan para can be reached only by a pedestrian path for about 3 km from Pattayakkudy, in Vannappuram Panchayath in Idukki district. Cochin Port and parts of Thrissur district can also be seen from top of the Meenuliyan para.</p><br>
<p>Kfar Tebnit or Kfar Tibnit  is a village located approximately 4 km south southeast of Nabatieh, 37 km southeast of Sidon in Lebanon.</p><br>
<p>Kfar Tebnit takes its name from Tabnith (Hebrew "Tibni"), a ruler in the area ca. 280 BC and known as the "king of two Sidons". The sarcophagus of his son Eshmun-&#39;azar was found to bear a long inscription aimed to prevent looting with assurances that the tomb contained no treasure.</p><br>
<h2>Archaeology</h2><br>
<p>A Heavy Neolithic archaeological site of the Qaraoun culture was discovered here in 1926 by E. Passemard. Heavy Neolithic materials were found alongside one Trihedral Neolithic along with more regular Neolithic pieces. The tools were in sharp condition, made of fresh chert or grey-green flint and are stored in the National Museum of Beirut.</p><br>
<h2>History</h2><br>
<p>In 1875 Victor Guérin visited, and found here 130 Metualis.</p><br>
<p>Guphapokhari is a natural pond situated at the height of 2,890 m</p><br>
<p>above the sea levels situated in Gufa VDC of Sankhuwasabha District of Nepal. This beautiful lake is also a holy pilgrimage site for both Hindus and Buddhists. The name "Guphapokhari", which means Cave Pond, is a new name given to this about 50 years ago, by Sages and priests who were believed to meditate in the caves around the hills of this area and gave it its new name. Previously, it was called "Siddha Marga" Pokhari. Locals believe that this pond grants your wishes, similar to the Manakamana Temple in Gorkha.</p><br>
<p>Guphapokhari is one of the most popular destinations in the Tinjure Milke Jaljale Trail, which is famously known as the "Rhododendron capital of Nepal". This region boasts the highest number of Rhododendron Species, 28 out of 32 found in Nepal. Not to mention thousands of other flowers and plants, hundreds species of birds, numerous species of Mammal and the magnificent view of Makalu, Kanchanjunga and Mt. Everest on a clear day. The reflection of the tree, and the mountain ranges is one of the most iconic view of this location. On a clear night, photographers have been able to capture the milkyway reflection on this pond.</p><br>
<p>Delaware, Lackawanna and Western Railroad Yard-Dickson Manufacturing Co. Site is a national historic district located in Scranton, Lackawanna County, Pennsylvania. It encompasses the Steamtown National Historic Site and Scranton Army Ammunition Plant and includes 16 contributing buildings, four contributing sites, and five contributing structures. The yard includes buildings and structures related to the yard&#39;s expansion in 1899-1939, and its usage as steam locomotive maintenance complex. The Dickson Manufacturing Company built steam locomotives, and the site of its works are included in this district.</p><br>
<p>Notable buildings at the Steamtown National Historic Site include the following:</p><br>
<p>Gas House (1909)</p><br>
<p>Office and Storage Building (1909)</p><br>
<p>Green Sands Storage Bin and Dryer (1917)</p><br>
<p>Oil House (1912)</p><br>
<p>Maintenance Shop (1865–1949)</p><br>
<p>Roundhouse Office and Storeroom (1902)</p><br>
<p>Roundhouse remnants (1902, 1937)</p><br>
<p>Mattes Street Signal Tower (1908) and Warehouse (1876, 1901, 1926).</p><br>
<p>Notable buildings at the Scranton Army Ammunition Plant include the following:</p><br>
<p>Pattern Shop/Office Building (1907–1909)</p><br>
<p>Foundry/Forge Shop (1907–1909)</p><br>
<p>Blacksmith Shop/Heat Treat Building (1907–1909)</p><br>
<p>Machine and Erecting Shop/Production Shop (1907–1909).</p><br>
<p>Note: This includes and</p><br>
<p>It was added to the National Register of Historic Places in 1990.</p><br>
<p>Manda Hararo is a group of basaltic shield volcanoes in east Africa whose last eruption was in 2009. The group is very large, spreading over 105 km&sup2;. At its northern end is a small example. South of this volcano is the Gumatmali-Gablaytu fissure system, an area dominated by fissure-fed lava flows. At the centre of the complex rise two volcanoes. Manda Hararo&#39;s large size is because it is a raised block from the end of a mid-ocean ridge spreading center. It is known for its rare basalts.</p><br>
<h2>Eruptions</h2><br>
<h3>2007 eruption</h3><br>
<p>Manda Hararo first erupted on August 13, 2007. NASA&#39;s Aura Satellite detected a large sulfur dioxide plume over Ethiopia and Sudan. Satellite imagery showed a lava flow emitted by Manda Hararo. Local residents reported that no precursors to the eruption had taken place. The first sign was a sudden, heavy, cracking sound, with only a slight tremor. At 17:30, fire was seen coming from Manda Hararo, "lighting up the entire area." Locals evacuated while the violent eruptions continued for three days. After the main eruption, lava flows continued and much of the fissure gave off strong fumarolic activity. On August 20, a team of scientists visited the area.</p><br>
<h3>2009 eruption</h3><br>
<p>On 29 June another plume was detected from the same area. Imagery showed thermal anomalies coming from Manda Hararo. A team of field scientists reached the site on 4 July and found the eruption had produced basaltic lava flows from fissures 4 – long. The fissures were lined by scoria ramparts. The eruption was possibly bigger than the 2007 eruption. By the time the scientists reached the fissure, it only emitted steam.</p><br>
<p>The Co-operative Block Building is a commercial structure in downtown Crawford, Nebraska. It was built in 1909 and added to the National Register of Historic Places on September 12, 1985. It is also known locally as Co-op Block, Midwest Block, or The Ranch House, after the business that it currently houses.</p><br>
<h2>Description</h2><br>
<p>The Co-operative Block Building is a two-story Victorian commercial edifice in Crawford at the northwest corner of 2nd and Linn Streets on lots 9, 10, 11, and 12 of block 10 of the original townsite. It was built in 1909 of reinforced concrete and has plastered exterior walls; however, the interior structure utilized a wooden infrastructure. The edifice is square in shape, at 100 ft by 100 ft, and has a relatively flat roof. The front (east) facade is symmetrically organized and divided into four bays, a division which is further achieved inside the building. The storefronts have been replaced since the original construction (although they still consist mainly of glass), and some of the upper-story windows have been filled in. The facade is topped by a pressed metal cornice with brackets designed to look like dentils. Although a sign inscribed with the buildings name originally embellished the top of the structure, it has since been removed, along with other cornice embellishments. There is a basement entrance on the buildings south side.</p><br>
<h2>History</h2><br>
<p>The Crawford Co-operative Company was founded on June 11, 1907 by William J. A. Raum, C. H. Britton, W. A. Eversull, Bernard Soester, J. H. Hulseman, and Edwin Kluman. The purpose of the organization was to be "the buying, selling and holding of real estate, engaging in the general merchandise business, the buying and selling of all kinds of farm products, poultry and eggs". The Company officially began business on July 9, 1907; its capital stock was worth $100,000. On April 14, 1908 the company approved the plans and specifications submitted by William Stanton & Sons for the construction of the present Co-operative Block Building. Although it was originally to be built with its floors and roof entirely of concrete, the interior infrastructure was ultimately built using slow-burning heavy mill construction. Erected in 1909, the Co-operative Block Building was the first building to use reinforced concrete construction in the Crawford area. The Company dissolved in 1977.</p><br>
<p>The structure has been occupied by a grocery store, a funeral parlor, and Midwest Hardware. It was also used for offices, apartments, and a meeting space for the Ku Klux Klan. A 1939 fire, thought to originate in the basement, caused considerable damage to the building, although no casualties occurred. In 1978 a restaurant, ODohertys, was opened in the building by Tom and Donna Spence. The structure was refurbished, and a back bar from a historic saloon in Summit, South Dakota was added. Some of the new furbishing came from the Crawfords former Gate City Hotel. Later, the business was acquired by Butch and Becky Sellman, who in turn sold it to the Kreman family. The restaurant is currently in operation as MJs Ranch House. Also occupying the Co-operative Block is the Crawford Clipper, the local newspaper.</p><br>
<p>The Cordillera Vilcanota  is a mountain range located in Peru southeast of Cusco, on the boundary between the regions of Cusco and Puno. It extends between 13°39 and 14°29S and 70°31 and 71°20W for about 80 km. It includes 469 glaciers.</p><br>
<p>To the east the rivers San Gabán and Azángaro are the natural boundary which separates it from the Carabaya range. The La Raya range near the La Raya pass is sometimes included or listed separately.</p><br>
<h2>Toponyms</h2><br>
<p>Most of the names in the range originate from Quechua and Aymara. They used to be spelled according to a mainly Spanish-based orthography which is incompatible with the normalized spellings of these languages and Law 29735 which regulates the use, preservation, development, recovery, promotion and diffusion of the originary languages of Peru. According to Article 20 of Decreto Supremo No 004-2016-MC (Supreme Decree) which approves the Regulations to Law 29735, published in the official newspaper El Peruano on July 22, 2016, adequate spellings of the toponyms in the normalized alphabets of the indigenous languages must progressively be proposed with the aim of standardizing the namings used by the IGN. The IGN realizes the necessary changes in the official maps of Peru. These changes are part of a process to promote the indigemous languages and to reassert the rights of the indigenous peoples.</p><br>
<p>Hints to wrong spellings are terms containg hua and hui (instead of wa and wi), "e", "o", "ca", "cu", "qu" or diphthongs among others.</p><br>
<h2>Mountains</h2><br>
<p>The highest mountain in the range is Ausangate which is also the fourth largest mountain in Peru. Other notable peaks including the Ayakachi group, the northern extension of the range, are listed below:</p><br>
<p>Callangate, 6,110 m</p><br>
<p>Chumpe, 6,106 m</p><br>
<p>Alcamarinayoc, 6,102 m</p><br>
<p>Jatunhuma, 6,093 m</p><br>
<p>Yayamari, 6,049 m</p><br>
<p>Huiscachani, 6,000 m</p><br>
<p>Huila Aje, 5,900 m</p><br>
<p>Japu Punta 5,850 m</p><br>
<p>Jatunñaño Punta 5,812 m</p><br>
<p>Condoriquiña, 5,780 m</p><br>
<p>Joyllor Puñuna, 5,743 m</p><br>
<p>Kiru (or Sallqantay), 5,720 m</p><br>
<p>Awsanqati, 5,714 m</p><br>
<p>Quishuarnioj, 5,700 m</p><br>
<p>Quevesere, 5,700 m</p><br>
<p>Kisu Q&#39;ipina, 5,650 m</p><br>
<p>San Braulio, 5,650 m</p><br>
<p>Iskupitani, 5,600 m</p><br>
<p>Puca Punta, 5,600 m</p><br>
<p>Hualipayoc, 5,600 m</p><br>
<p>Jonorana, 5,553 m</p><br>
<p>Cóndor Tuco, 5,550 m</p><br>
<p>Huayruro Punco, 5,550 m</p><br>
<p>Jolljepunco, 5,522 m</p><br>
<p>Pomanota, 5,516 m</p><br>
<p>Japu Japu, 5,500 m</p><br>
<p>Millo, 5,500 m</p><br>
<p>Uriyuq, 5,500 m</p><br>
<p>Osjollo Anante, 5,500 m</p><br>
<p>Yanajaja, 5,500 m</p><br>
<p>Cinajara, 5,471 m</p><br>
<p>Ayakachi, 5,470 m</p><br>
<p>Pantipata, 5,450 m</p><br>
<p>Quinsachata, 5,442 m</p><br>
<p>Quyllur Rit&#39;i, 5,402 m</p><br>
<p>Apu K&#39;uchu, 5,400 m</p><br>
<p>Chilinita, 5,400 m</p><br>
<p>Jatun Quenamari 5,400 m</p><br>
<p>Jatuncucho 5,400 m</p><br>
<p>Istalla, 5,400 m</p><br>
<p>Jarupata, 5,400 m</p><br>
<p>Cuncapata 5,400 m</p><br>
<p>Cuncunani 5,400 m</p><br>
<p>Mullucocha, 5,400 m</p><br>
<p>Pucasalla, 5,400 m</p><br>
<p>Pajo, 5,400 m</p><br>
<p>Ccolcce, 5,400 m</p><br>
<p>Comercocha, 5,400 m</p><br>
<p>Sacsa Ananta, 5,400 m</p><br>
<p>Huasacocha, 5,400 m</p><br>
<p>Jatun Alfapata, 5,390 m</p><br>
<p>Qillita, 5,386 m</p><br>
<p>Waykintani, 5,350 m</p><br>
<p>Jachatira, 5,320 m</p><br>
<p>Pucacocha, 5,320 m</p><br>
<p>Otoroncane, 5,305 m</p><br>
<p>Ananta 5,300 m</p><br>
<p>Chaupimaquito, 5,300 m</p><br>
<p>Chuallani, 5,300 m</p><br>
<p>Uchuy Milla, 5,300 m</p><br>
<p>Jampatune, 5,300 m</p><br>
<p>Aquichua, 5,300 m</p><br>
<p>Cunorana, 5,300 m</p><br>
<p>Quellhuacota, 5,300 m</p><br>
<p>Cochacucho, 5,300 m</p><br>
<p>Quehuesiri, 5,300 m</p><br>
<p>Sanimayo, 5,300 m</p><br>
<p>Sullulluni, 5,300 m</p><br>
<p>Surapata, 5,300 m</p><br>
<p>Suyuparina, 5,300 m</p><br>
<p>Unollocsina, 5,300 m</p><br>
<p>Huisahuisa, 5,300 m</p><br>
<p>Jupucunca, 5,295 m</p><br>
<p>Tocllayoc, 5,291 m</p><br>
<p>Culi, 5,290 m</p><br>
<p>Minasnioc, 5,248 m</p><br>
<p>Huampuni, 5,248 m</p><br>
<p>Ananta, 5,200 m</p><br>
<p>Chullumpina, 5,200 m</p><br>
<p>Hatun Punta, 5,200 m</p><br>
<p>Jatun Sallica, 5,200 m</p><br>
<p>Inkaqucha, 5,200 m</p><br>
<p>Kimsa Chata, 5,200 m</p><br>
<p>Kuntur Sayani, 5,200 m</p><br>
<p>Llusca Ritti (in Corani), 5,200 m</p><br>
<p>Llusca Ritti, 5,200 m</p><br>
<p>Macho Ritti, 5,200 m</p><br>
<p>Pariyuq, 5,200 m</p><br>
<p>Pata Q&#39;ispi Kancha, 5,200 m</p><br>
<p>Pichacani, 5,200 m</p><br>
<p>Jori Pintay, 5,200 m</p><br>
<p>Conatira, 5,200 m</p><br>
<p>Catautira, 5,200 m</p><br>
<p>Runcu Tauja, 5,200 m</p><br>
<p>Sallatira, 5,200 m</p><br>
<p>Sambo, 5,200 m</p><br>
<p>Sayrecucho, 5,200 m</p><br>
<p>Surimani, 5,200 m</p><br>
<p>Taruca Sayana, 5,200 m</p><br>
<p>Tutallipina, 5,200 m</p><br>
<p>Orco Puñuna, 5,200 m</p><br>
<p>Othaña, 5,200 m</p><br>
<p>Waman Lipani, 5,200 m</p><br>
<p>Huamanripayco, 5,200 m</p><br>
<p>Huanacune, 5,200 m</p><br>
<p>Huancane Apacheta, 5,200 m</p><br>
<p>Huarisayana, 5,200 m</p><br>
<p>Viluyo, 5,200 m</p><br>
<p>Hueco, 5,200 m</p><br>
<p>Yanajasa, 5,200 m</p><br>
<p>Culipata, 5,172 m</p><br>
<p>Pucajasa, 5,165 m</p><br>
<p>Cóndor Sallani, 5,102 m</p><br>
<p>Ananta Cucho, 5,100 m</p><br>
<p>Ancahuachana, 5,100 m</p><br>
<p>Ancahuachanan, 5,100 m</p><br>
<p>Chachacumani, 5,100 m</p><br>
<p>Chachacomayoc, 5,100 m</p><br>
<p>Jarjapata, 5,100 m</p><br>
<p>Mamanlipani, 5,100 m</p><br>
<p>Piyacuyani, 5,100 m</p><br>
<p>Quello Cunca, 5,100 m</p><br>
<p>Riticocha, 5,100 m</p><br>
<p>Sallaqucha, 5,100 m</p><br>
<p>Huilacunca, 5,100 m</p><br>
<p>Velacota, 5,100 m</p><br>
<p>Huillopuncho, 5,100 m</p><br>
<p>Yana Orjo, 5,100 m</p><br>
<p>Intijahuana, 5,099 m</p><br>
<p>Alcamarina, 5,085 m</p><br>
<p>Viscachani, 5,065 m</p><br>
<p>Sumpiruni, 5,063 m</p><br>
<p>Comercocha, 5,060 m</p><br>
<p>Quenamari, 5,054 m</p><br>
<p>Piscopata, 5,037 m</p><br>
<p>Sillajata, 5,037 m</p><br>
<p>Yanacocha, 5,025 m</p><br>
<p>Chiajarjapata, 5,014 m</p><br>
<p>Anta Punco, 5,000 m</p><br>
<p>Chachacumani, 5,000 m</p><br>
<p>Chojorusi, 5,000 m</p><br>
<p>Jatunrritioc, 5,000 m</p><br>
<p>Hatun Sallayuq, 5,000 m</p><br>
<p>Hatun Tiyana, 5,000 m</p><br>
<p>Jatunyurac Caca, 5,000 m</p><br>
<p>Illaq Urqu, 5,000 m</p><br>
<p>Kuntur Sayana, 5,000 m</p><br>
<p>Jairani 5,000 m</p><br>
<p>Pata Anjasi, 5,000 m</p><br>
<p>Pirhuani, 5,000 m</p><br>
<p>Pucachuaña, 5,000 m</p><br>
<p>Pisquioc, 5,000 m</p><br>
<p>Collpacaja (Puno), 5,000 m</p><br>
<p>Collpacaca, 5,000 m</p><br>
<p>Colquetauca, 5,000 m</p><br>
<p>Quello Sallayoc, 5,000 m</p><br>
<p>Quello Huallayoc, 5,000 m</p><br>
<p>Q&#39;umirqucha, 5,000 m</p><br>
<p>Riti Huasi, 5,000 m</p><br>
<p>Salla Huancane, 5,000 m</p><br>
<p>Sihuarani, 5,000 m</p><br>
<p>Soracucho, 5,000 m</p><br>
<p>Tarucani, 5,000 m</p><br>
<p>Tocra, 5,000 m</p><br>
<p>Ojecunca, 5,000 m</p><br>
<p>Huillolluni, 5,000 m</p><br>
<p>Yanacucho, 5,000 m</p><br>
<p>Yana Sallayoc, 5,000 m</p><br>
<p>Yana Urqu, 5,000 m</p><br>
<p>Yanaqucha (in Carabaya), 5,000 m</p><br>
<p>Yanacocha (Carabaya-Melgar), 5,000 m</p><br>
<p>Yuracjasa, 5,000 m</p><br>
<p>Yurac Salla, 5,000 m</p><br>
<p>Yurac Huayruro, 5,000 m</p><br>
<p>Chiaraje (Cusco-Puno), 4,900 m</p><br>
<p>Chiaracce (Melgar), 4,900 m</p><br>
<p>Puicutuni, 4,900 m</p><br>
<p>Queullacocha, 4,900 m</p><br>
<p>Jolpajaja, 4,900 m</p><br>
<p>Huayruruni, 4,900 m</p><br>
<p>Huiscana, 4,900 m</p><br>
<p>Chiriunuyoc, 4,800 m</p><br>
<p>Hatun Wayq&#39;u, 4,800 m</p><br>
<p>Huch&#39;uy Ananta, 4,800 m</p><br>
<p>Jaquehuata, 4,800 m</p><br>
<p>Condorsenja, 4,800 m</p><br>
<p>Pirhuane, 4,800 m</p><br>
<p>Pucaparina, 4,800 m</p><br>
<p>Jajachaca, 4,800 m</p><br>
<p>Queljata, 4,800 m</p><br>
<p>Tipajasa, 4,800 m</p><br>
<p>Urqu Puñuna, 4,800 m</p><br>
<p>Waracha, 4,800 m</p><br>
<p>Huayllahuito, 4,800 m</p><br>
<p>Vilapata, 4,800 m</p><br>
<p>Vilacirca 4,800 m</p><br>
<p>Yana Urqu, 4,800 m</p><br>
<p>Yana Urqu, 4,800 m</p><br>
<p>Yuraq Q&#39;asa, 4,800 m</p><br>
<p>Quechajaja, 4,600 m</p><br>
<p>Jollpajaja, 4,600 m</p><br>
<p>Yuracjaja, 4,600 m</p><br>
<h2>Lakes</h2><br>
<p>Sibinacocha is the largest of about 22 lakes in the range followed by Lake Singrenacocha northwest of it. Other notable lakes are Armaccocha, Jatun Pucacocha, Pucacocha and Huarurumicocha.</p><br>
<p>Achabal Garden is one of the most important and splendid tourist places in the state of Kashmir and is about 8 kilometers away from Anantnag. It was in the state of Kashmir that the Mughal style gardens was brought to perfection and Achabal is one such masterpiece. This place is famous all over due to an ancient spring surrounded by a terrace garden, which was developed by Mughals. The historical significance of this place strikes the visitor with awe.Achabal Garden, once the pleasure retreat of the Mughal Empress Noor Jahan is a beautifully created garden in Kashmir with its own special allure and character. Its picturesque beauty makes it one of the best Mughal gardens of the Indian subcontinent. It is difficult to describe in words the mesmerizing beauty of this Mughal style garden. The upper portion of the garden is popularly known as `Bag-e-Begum Abad` and was developed by Malika Noor Jehan Begum in 1620 A.D. Later it became renowned as Sahib Abad in which there was a `Hamam` or treasure of water getting heat from a logical lamp or `tosng`. The garden was created at the site of a powerful spring, which enters the garden as a waterfall. The design of this wonderfully created garden is ascribed to the beloved wife of the Mughal Emperor Jahangir. The Garden of Achabal is located at the foot of a hill covered with dense forest, which is 8 kilometers from Anantnag and 56 kilometers from Srinagar. The daughter of the Mughal monarch Shah Jahan built the garden in the year 1620 with cascading outpourings and pavilions. The most beautiful of all springs is Achabal and it gushes out of the Sosanwar Hill. In the garden of Achabal the water gushes out of the spasm with great vigor throughout the entire year. In the later ages the Mughal prince Dara Shikoh built a mosque in the garden. There is also a trout farm for seed fish nearby. There are tourist bungalows and tourist huts nearby where the tourists can spend some moments in the lap of the beautiful setup. This garden is universally regarded as a visual treat for the eyes. This garden is also well adorned with sprawling Chinar trees. Stepped terraces, ornamental shrubs and conventional elegance, are the added attraction, which not only mesmerizes one but also attracts thousands of tourists from all over the globe every year. Accommodation is available at the nearby tourist bungalows or rest houses. Achabal not only serves as a breathtaking splendor but also is a reviving experience for all tourists.</p><br>
<p>Achabal Gardens, "the places of the princes", is a small Mughal garden located at the southeastern end of the Kashmir Valley in the town of Achabal, Anantnag district, India. Located near the Himalayan Mountains, the site may have been a Hindu sacred site known as "Akkshavala" previously.</p><br>
<h2>Overview</h2><br>
<p>It was built about 1620 A.D. by Mughal Empire Emperor Jahangir&#39;s wife, Nur Jahan, called the "greatest garden lovers of them all." The garden was rebuilt on smaller scale by Gulab Singh and is now a public garden.</p><br>
<p>A main feature of the garden is a waterfall that enters into a pool of water.</p><br>
<p>This place is also noted for its spring, which is finest in Kashmir and is supposed to be the re-appearance of a portion of the river Bringhi, whose waters suddenly disappear through a large fissure underneath a hill at the village Wani Divalgam in the Brang Pargana. It is said that in order to test this, a quantity of chaff was thrown in the Bringhi river at a place its water disappears at Wani Divalgam and that chaff came out of the Achabal spring. The water of the spring issues from several places near the foot of a low spur which is densely covered with deodar trees and at one place it gushes out from an oblique fissure large enough to admit a man&#39;s body and forms a volume some 18 inches high and about a foot in diameter.</p><br>
<h2>Business</h2><br>
<p>Time 2 Taste Restaurant</p><br>
<p>Mughal View Restaurant</p><br>
<p>Raja Hotel</p><br>
<p>Zaiqa Restaurant</p><br>
<p>Amir Telecom</p><br>
<p>The Boulder Mountains are part of the Rocky Mountains in the western United States. Located in central Idaho, they stretch from a few miles north of Ketchum to north to near Challis, and part of the range is within the Sawtooth National Recreation Area and partially within the Hemingway–Boulders Wilderness. The highest point in the range is Ryan Peak.</p><br>
<p>During the summer popular hiking destinations include the many trails in the southern section of the Boulder Mountains where many of the highest peaks are located. The front of the Boulder Mountains are close to, and clearly visible from, State Highway 75, the Sawtooth Scenic Byway. Here along the Big Wood River forests exist along the base of the mountains, while the northern extent of the range has much more sagebrush.</p><br>
<p>Part of the 1985 movie Pale Rider was filmed in the Boulder Mountains.</p><br>
<h2>Peaks</h2><br>
<h2>Lakes</h2><br>
<p>The Houghton Fire Hall, officially called the Continental Fire Company Building, Built in 1883, it was the original home of the Michigan Mining School and is a Michigan State Historic Site.</p><br>
<h2>History</h2><br>
<p>The Continental Fire Company organized in 1860 in Houghton. The department&#39;s first fire hall was built in 1861 along the waterfront near the site of the modern-day Portage Lake Lift Bridge.</p><br>
<p>The new fire hall was built in 1883 Village offices were on the second floor. The Michigan Mining School, now Michigan Technological University, held its first classes on the second floor and in the basement from 1886 through May 1889. In the early 1900s, the building was extended to the north to store more oats and hay for the horses. In 1916, an addition was built on the western side to store two more fire engines.</p><br>
<p>The city moved its offices out of the fire hall in the 1930s. The fire bell was removed in October 1975 and transferred to the new location. The western addition was sold and became an auto supply store.</p><br>
<p>The fire hall was listed as a Michigan State Historic Site on August 6, 1976. The western addition became vacant in October 2011 when the auto supply store moved to a new location.</p><br>
<h2>Architecture</h2><br>
<p>The fire hall is a flat-roofed, three-story brick structure designed in the Italianate style. The foundation is built of rubble and painted white. A small, four-faced clock tower was originally situated on the cupola at the front of the building. The vertical space provided room for fire hoses to hang and dry.</p><br>
<p>Bethel Church is a historic church building in rural Morning Sun, Iowa, United States. The congregation was organized by the Wapello mission of the Methodist Episcopal Church in Iowa in 1854. In addition to the Morning Sun congregation, the Wapello mission included congregations in Concord, Long Creek, and two in Wapello. The property for the church building and its adjacent cemetery was donated by Merit Jamison. Members of the congregation built the building under the supervision of stonemason Francis McGraw. The limestone structure is a Vernacular form of Iowa folk architecture. The small cornice returns are influenced by the Greek Revival style. The plain interior features plastered walls, plank flooring and wood-carved furnishings from the church&#39;s early years. The iron fence that runs along the gravel road was added in 1861. The church is no used for regularly scheduled services. It was added to the National Register of Historic Places in 1979.</p><br>
<p>Union Church, also known as Brick Church, is a historic church building located in Davis City, Iowa, United States. For the first 20 years of its existence Davis City did not have a church. This church was built at the instigation</p><br>
<p>of John Clark in 1878. Clark was a native of Scotland who was of no particular religious affiliation, but thought "the moral and religious training</p><br>
<p>of the Christian faith of fundamental importance." The church building was accessible to all denominations, and is now owned jointly by Methodist, Presbyterian, and Christian congregations. It was added to the National Register of Historic Places in 1976.</p><br>
<p>The 36 by brick structure features a clock and bell tower on its front facade. The bell is mounted on the outside of the tower. Entry doors, with fan lights, flank the tower. Roman arch windows are used throughout the building.</p><br>
<p>Waiowa  is an isolated trachyandesitic volcano on New Guinea island, Papua New Guinea. It is located 19 km inland from Collingwood Bay in Oro Province. It lies on a fault line along the northeast flank of the Owen Stanley metamorphic belt. It is one of the planet&#39;s newest volcanoes, it formed in September 1943.</p><br>
<h2>1943-1944 eruption</h2><br>
<p>After four months of volcanic earthquakes, small phreatic eruptions began on 18 September 1943, breaking through a layer of highly metamorphosed rocks, before the first major explosion occurred on 27 December 1943. Two more major explosions occurred on 13 February and 23 July 1944, creating pyroclastic flows and lahars, and leveling 80 km of forest. The eruption stopped on the final explosion on 31 August 1944. The volcano was capped with a 500 m wide, steep-walled crater that is now forested and contains a small lake.</p><br>
<p>The Sidney D. Miller Middle School, also known as the Sidney D. Miller Junior High and High School, is a school building located at 2322 DuBois Street in Detroit, Michigan. It served as a high school from 1933 to 1957, and was significant as the de facto high school serving African American students in Detroit. It was designated a state of Michigan Historic Site in 1986 and was listed on the National Register of Historic Places in 2011.</p><br>
<h2>History</h2><br>
<p>Detroit experienced a phenomenal increase in population during the 1910s. To accommodate the influx of residents and their children, numerous schools were built during the decade. Ground was broken for what was then called the "Dubois School" in 1918; the school was intended to serve as a junior high. The school was designed by the architectural firm of Malcomson and Higginbotham, the architects of nearly all Detroit Public Schools in the period 1894 to 1923, and constructed at a cost on $245,616. However, construction plans were changed several times, and the school was not opened to students until 1921. The building itself was finally completed in 1922.</p><br>
<p>During the 1920s, the citys population continued to grow, stretching the capacity of the school system. An addition to Miller, including a girls gymnasium, was completed in 1931. Although the area around the school was predominantly white when the building opened, the percentage of African Americans in the Black Bottom neighborhood increased so that soon it was predominantly black. Parents of white students at nearby Eastern High School complained about the rising Black student population, and in response the Detroit School Board converted Miller to a senior high school in 1933. A liberal school transfer policy allowed white students zoned to Miller to attend Eastern, which left Miller as the de facto, if not de jure, African-American High school.</p><br>
<p>The school is significant in part because of its association with the education of African American students, beginning in 1933. Due in part to concerns from the black community, the School Board installed a number of Black teachers and administrators at Miller. However, in 1955, steps were taken to end the de facto segregation of the Detroit School system, and in 1957 the building was converted back into a middle school. It remained a middle school for 50 years, and was closed in 2007.</p><br>
<h2>Athletics</h2><br>
<p>Miller High School met Detroit St. Joseph High School in 1947 at Detroit&#39;s Olympia Stadium in what became the first City Basketball Championship game in Detroit PSL and Catholic High School League history. Miller won that game 47 to 34 before a Michigan high school record attendance of 11,563.</p><br>
<h2>Description</h2><br>
<p>The Miller School is a 2-1/2 story Jacobethan building with a flat roof, built of red brick with limestone beltcourses. The front (west) and rear façades are asymmetrical, with three-story projecting bays. The entrance is through a Gothic arch flanked by piers; the words "SYDNEY D. MILLER JUNIOR HIGH SCHOOL AD 1919" are carved above the entrance. The original 1921 building occupies an L-shaped footprint. Later additions in 1931 and 1951 extended the building further east and enclosed a small courtyard within the building, making the perimeter nearly rectangular.</p><br>
<p>The Edmund Atkinson School is a school building located at 4900 East Hildale Street in Detroit, Michigan. It is currently operating as Legacy Charter Academy. It was listed on the National Register of Historic Places in 2011.</p><br>
<h2>History</h2><br>
<p>Edmund Atkinson was a Detroit lawyer who served on the city council from 1900 to 1904, and worked as Assistant Corporation Council for the city and for the Detroit Board of Education. His namesake, the Edmund Atkinson School, was designed as a multi-unit school by the architectural firm of McGrath, Dohmen, & Page. The first unit was built in 1927 with a capacity for 580 pupils in kindergarten through eighth grade. It opened the following year, serving students who were primarily first generation immigrants from Eastern European or the Middle East, as well as African American students.</p><br>
<p>The second unit, unit, containing an auditorium, gymnasium, practical arts room, three classrooms and a combination lunch/playroom, was</p><br>
<p>built in 1931. The third unit planned by McGrath, Dohmen, & Page was never built; however, a temporary building with two self-contained classrooms was installed in 1955, and by 1961, the school was serving 880 students in kindergarten through sixth grade The new owners invested $6 million to renovate the building, and reopened it in the fall of 2010 as Legacy Charter Academy.</p><br>
<h2>Description</h2><br>
<p>Atkinson School was built as two major units. The original 1927 unit is a two-story symmetrical orange-brick and random range ashlar, Collegiate Gothic Revival structure five bays wide. The central entrance bay has a projecting entrance vestibule on the first floor with a compound Gothic arch above. The flanking bays contain large openings with groupings of windows, while the outer bays contain a single window opening per floor. The side of the building contains nine bays and a single entrance.</p><br>
<p>The connecting 1931 unit, also of orange brick, begins at the end of the nine-bay span of the first unit with a tower-like bay containing groupings of windows and a third entrance. The unit continues with a two-story rear elevation. All entrances and towers have limestone surrounds and quoining.</p><br>
<p>Armutlu Peninsula  is a peninsula extending westward into Marmara Sea in the Anatolian section of Turkey. In addition to Yalova Province, parts of Kocaeli Province and Bursa Province are on the peninsula.</p><br>
<h2>Geography</h2><br>
<p>Armutlu Peninsula is between Gulf of Izmit in the north and Gulf of Gemlik in the south. The westernmost point of the peninsula is the cape of Bozburun. The bird&#39;s flight distance between Bozburun and the tip of the northern gulf is about 100 km. But, the distance between Bozburun and the tip of the southern gulf is only about 30 km. To the southeast of the peninsula, Lake İznik is situated.</p><br>
<p>The peninsula is actually a part of Samanlı Mountains, a mountain range lying between Bolu Mountains and Bozburun. The peak of the mountains within the peninsula is Taz Mountain with an altitude of 921 m. The mountains are covered with forests.</p><br>
<h2>Notable places</h2><br>
<p>Yalova, central city of the Yalova Province is at the northern coast. Most district centers of the province are in the coastal area of the peninsula. The peninsula is named after Armutlu district. Gölcük, a town in Kocaeli Province, best known for the Turkish Navy&#39;s main naval base with shipyard and the Ford Otosan automobile plant, is located at the northern gulf of the peninsula. Also on the northern coastline between Gölcük and Yalova, Karamürsel is located in Kocaeli Province. Historically, it was an important Ottoman naval base and during the Cold War era, the town hosted a United States naval air station, which operated a special antenna to intercept Soviet Union radio transmissions. West of Yalova, Çınarcık is located, a well-known seaside resort.</p><br>
<p>Another notable location is Gemlik, a district of Bursa Province, situated at the peninsula&#39;s southern gulf. An important port city, it is renowned for its olives and olive oil.</p><br>
<p>The population density in the mountains at the inner peninsula is low, where there are only small villages.</p><br>
<h2>Geology</h2><br>
<p>Both gulfs at the north and the south are actually on two active tectonic fault lines. The entire peninsula was hit by the İzmit earthquake on August 17, 1999 that occurred along the western portion of the North Anatolian Fault Zone.</p><br>
<p>The Duane Doty School is a school building located at 10225 3rd Street in Detroit, Michigan. It was listed on the National Register of Historic Places in 2011.</p><br>
<h2>History</h2><br>
<p>The Duane Doty School was named after former Superintendent of Schools for Detroit Duane Doty, who was appointed to that post in 1865. and ending in 1909. When it opened, the school contained 20 classrooms and was intended to hold 640 students from kindergarten through eighth grade. which added 320 students to the school&#39;s capacity. A gymnasium addition was constructed in 1928. In 1959, the building was substantially remodeled, and six new classrooms were added in the basement and first floor. By the end of 1960, enrollment in the school was 1,193 students.</p><br>
<p>The building was later used as the Boykin Continuing Education Center. After major renovations completed in 2012, the building was re-opened as The Henry Ford Academy: Elementary School.</p><br>
<h2>Description</h2><br>
<p>The Duane Doty School is a two-story L-shaped, red brick, hipped roof structure placed on a high, windowed basement. The front facade has five bays, with the central bay projecting substantially outward. The two main entrances are located in single story vestibules flanking the main bay. The central and end bays of the school contain rows of wooden six-over-six sash windows with stone sills. The roof eaves are supported by paired or triples sets of oversized decorative brackets. A square tower behind one of the entrances pierces the roofline. A hipped roof addition dating from 1921 sits behind the building, and the flat-roofed gymnasium from 1928 extends further.</p><br>
<p>Inside the building, the main entry vestibules have terrazzo floors, with stair cases leading up to the first floor. The original L-shaped building has two intersecting corridors leading to classrooms. The kindergarten classrooms are located between the two main entrances at the front of the building. The additions contain a one-story auditorium on the first floor with a gymnasium below in the basement.</p><br>
<p>Trinity Episcopal Church is a Gothic Revival-style Episcopal church at 205 East Montezuma Avenue in Houghton, Michigan. It was designated a Michigan State Historic Site on July 17, 1986. It is the second of two church buildings to exist on the site; the current one replaced a wooden structure in 1910. The church&#39;s philosophy is built on the Oxford Movement.</p><br>
<h2>History</h2><br>
<p>The parish was founded on July 17, 1860, when the Episcopal Bishop of Michigan, Reverend Samuel A. McCoskry, met with nine businessmen from Houghton and Hancock. The first clergyman sent to serve the church, upon arriving in Houghton on a Saturday, immediately departed on the vessel that had carried him. Public services were first held on September 15, 1860. The name Trinity Church was chosen at the first vestry meeting, held on July 13, 1861.</p><br>
<p>The church&#39;s first permanent home was a wooden building across the Portage Canal in Hancock, built on land donated by the Quincy Mining Company. However, it was soon decided that the structure would be moved to Houghton, on land owned by Shelden, a member of the church. The church was placed on a barge overnight, but it came free of its bounds and was found floating free in the morning. It was successfully recovered and transferred to Houghton, where it remained until 1910.</p><br>
<p>The wooden church was demolished in early 1910 to make way for the current church, built of brick and Jacobsville Sandstone, which was completed on Easter that same year. In 1995, a two-story addition was built to house the pastor&#39;s office. The current church was designated a Michigan State Historic Site on July 17, 1986, and an informational marker was erected on April 24, 1987.</p><br>
<h2>Architecture</h2><br>
<p>The church is a brick structure built in the Gothic Revival style. The basement façade, copings, and trim are all made of Jacobsville Sandstone. The building has a square tower at one corner capped with crenellations.</p><br>
<p>The building architect was John B. Sutcliffe and interior artwork and carvings were done by Alois Lang. The interior design of the church was influenced by the Oxford Movement. The roof&#39;s wooden trusses are exposed as arches that span the nave. The church houses an Austin Organ, opus 419, which was installed in 1913.</p><br>
<p>Laugerie-Basse is an important Upper Paleolithic archaeological site within the territory of the French commune Les Eyzies-de-Tayac-Sireuil in Dordogne. It is known for several works of art from the Magdalenian.</p><br>
<h2>Geography, Geology and Location</h2><br>
<p>The impressive Abri of Laugerie-Basse, named after the village, is located on the right side of the Vézère valley, about 2 kilometers upstream from Les Eyzies. It was formed at the bottom of a 45 meters high and 500 meters long scarp slope of flat-lying limestones from the Coniacian. The 15-meter-deep Abri is located 15 meters above river level. Taking advantage of the natural conditions, the houses of Laugerie-Basse were built directly into the rocks so that building a back wall and the back half of the roof was dispensable.</p><br>
<p>The prehistoric site consists of two abris: the main abri and 50 meters upstream the Abri of Marseilles.</p><br>
<p>Between the abris and the Vézère the D 47 runs from Périgueux to Les Eyzies.</p><br>
<h2>History</h2><br>
<p>In 1863 Édouard Lartet and Henry Christy began for the first time with excavations on the main abri. At that time a small farm with a barn and a stable was standing on the excavation area. Lartet and Christy were succeeded by the Marquis de Vibraye and his assistant Franchet and shortly thereafter by Massénat. The excavations on the main abri were rather chaotic for the next five decades. Only between 1912 and 1913 Denis Peyrony and Maury were able to proceed more systematically and make the first stratigraphy of the main abri. Maury then moved on to the hiterhto disregarded Abri des Marseilles where he was active until 1920.</p><br>
<h2>Stratigraphy</h2><br>
<p>The stratigraphy in the main abri comprises archaeological material mainly from Magdalenian III and Magdalenian IV. There is also some marginal evidence of the Azilian. In the slope waste in front of the scarp slope remains from the Neolithic and the late Bronze Age were also discovered.</p><br>
<p>The Abri de Marseilles offers a more detailed stratigraphic sequence: the original profile is still existing. From it one can conclude that the Magdalenians settled approximately 14,000 years ago directly on the existing bottom of the abri. They lived at the abri until the Magdalenian VI. Then a catastrophic collapse of the roof occurred and the settlement site was partly strewn with some huge slabs of rock and debris. Afterwards the people returned to this place, which is clearly evident from traces of settlement on and between the boulders. Thereafter the Abri des Marseilles sank completely into oblivion until the late Neolithic. Around 2000 BC members of the Artenac culture arrived who left an enormous, and in this magnitude inexplicable, ash and charcoal layer that covered the whole abri. Then further slides of the roof occurred bringing about a spectacular rock chaos with up to 10 meter high boulders.</p><br>
<p>By now the main abri has been cleaned up completely, whereas the Abri des Marseilles has only been partially explored.</p><br>
<h2>Found Artifacts</h2><br>
<p>Apart from stone artefacts and other tools, all in all approximately 600 art objects from the Magdalenian were recovered in Laugerie-Basse. In Laugerie-Basse Paul Hurault, 8th Marquis de Vibraye discovered in 1864 the "Immodest Venus" (French: Vénus impudique) which gave its name to the genre of paleolithic Venus figurines. Shortly after that, around 1867-68, the Woman under the reindeer (la femme au renne) was discovered by Abbé Landesque. A large part of these art objects is nowadays scattered in several museums all over the world. From the middle Magdalenian (stage IV) stem pierced bone rondels picturing chamoises and deer.</p><br>
<h2>Age</h2><br>
<p>The main abri was inhabited in the middle and upper Magdalenian as well as in the Azilian, which roughly corresponds to the time segment from 14,000 until 10,000 years BP.</p><br>
<p>The Abri des Marseilles has had a longer settlement period, it had been inhabited during the entire Magdalenian and into the Neolithic which corresponds to the time segment from 17,000 until 7,000 years BP.</p><br>
<p>Evergreen Cemetery is the city-maintained cemetery for Colorado Springs, Colorado, on the National Register of Historic Places in El Paso County, Colorado.</p><br>
<p>When Colorado Springs was founded in 1871 there were already two cemeteries serving El Paso County but both were quickly found to be inadequate in serving the needs of the rapidly growing city. In 1874, the founder of Colorado Springs, General William Jackson Palmer, founded a new cemetery two miles from town. The original names were the Mount Washington or Mountain Home Cemetery. In 1877, the name was changed to Evergreen Cemetery. In 1875, the original 10 acres or so was deeded to the city of Colorado Springs and it has been a city owned and operated cemetery since then. In 1993 the cemetery was placed on the National Register of Historic Places. The original 10 acres has grown to over 220 acres with 90,000 plus burials in 2014 and the cemetery still performs about 700 burials per year.</p><br>
<p>Evergreen Cemetery is the final resting place of many of the people that built the city of Colorado Springs along with founders of many neighboring cities. It is also the final resting place of many of the people that made millions from the last Colorado gold rush, world renowned artists, writers and composers, philanthropists, captains of industry and business, Union and Confederate soldiers, sports figures, politicians, actors, and even an astronaut.</p><br>
<h2>Notable Burials</h2><br>
<p>William Jackson Palmer (1836–1909), railroad builder, city father</p><br>
<p>Winfield Scott Stratton (1848–1902), mine owner, philanthropist</p><br>
<p>James Ferguson Burns (1853–1917), mine owner, philanthropist</p><br>
<p>Edward William Purvis (1857–1888), British officer and Hawaiian official</p><br>
<p>Francis Henry Maynard (1853–1926), cowboy, author</p><br>
<p>Franklin Eli Brooks (1860–1916), politician</p><br>
<p>Leo Arthur Hoegh (1908–2000), military figure</p><br>
<p>Helen Hunt Jackson (1830–1885), activist</p><br>
<p>Bob Johnson (ice hockey, born 1931) (1931–1991), hockey coach</p><br>
<p>Stan Keller (1907–1990), bandleader</p><br>
<p>Floyd K. Lindstrom (1912–1944), military figure</p><br>
<p>John Franklin Forrest (1927–1997), military figure</p><br>
<p>Robert Williamson Steele (1820–1901), territorial governor</p><br>
<p>Marshall Sprague (1909–1994), author</p><br>
<p>Dale Gardner (1948–2014), astronaut</p><br>
<p>Frederick Phillips Raynham (1893–1954), British aviator</p><br>
<p>Vic Heyliger (1912–2006), hockey player and coach</p><br>
<p>Harry Hunter Seldomridge (1864–1927), politician</p><br>
<p>Allen Tupper True (1881–1955), illustrator</p><br>
<p>Stephanie Westerfeld (1943–1961), figure skater</p><br>
<p>Andy Adams (writer) (1859–1935), writer</p><br>
<p>Pat Brady (1914–1972), actor</p><br>
<p>Irving Howbert (1846–1934), public servant, businessman</p><br>
<p>Sherman Coolidge (1862–1932), Episcopal Church priest, Indian advocate</p><br>
<p>Roland W. Reed (Royal Jr.) (1864–1934), artist, photographer</p><br>
<p>One Commonwealth war grave, of a Canadian Army soldier of World War I.</p><br>
<p>Amritavarshini Vav, also known as Panchkuva Stepwell or Katkhuni Vav, is a stepwell near the Panchkuva Darwaja in Ahmedabad, Gujarat, India.</p><br>
<h2>History</h2><br>
<p>Panchkuva, literally five wells, area derived its name the five wells in the area. Amritavarshini vav was completed in 1723 as per Devanagari and Persian inscription ( Vikram Samvat 1779/A.H. 1135 ) in the stepwell. It was built by Raghunathdas, diwan to Haidar Quli Khan, who was the governor of Gujarat during his stay in the city in 1721–1722 for charitable purpose.</p><br>
<h2>Architecture</h2><br>
<p>Sparsely ornamented, Amriavarshini Vav is notable for its L-shaped plan and has simple design. It has three storeys and is more than 50 feet deep. The bracing arches have different shapes at the two storeys and in the kuta (pavilion tower) before the well shaft. It was declared a protected monument in 1969 and was conserved in 1999. It was recharged later by digging in 2004.</p><br>
<p>Conger Mountain is a mountain in Millard County, Utah. It is located 60 miles west of Delta, Utah and is the highest peak in the Confusion Range.</p><br>
<h2>Wildlife</h2><br>
<p>Conger Mountain is almost completely undeveloped. It serves as a habitat for mule deer and antelope and is home to a herd of wild horses. It is considered a vital habitat for the golden eagle and bald eagles have been spotted near the mountain. Conger Mountain is also home to ferruginous hawks, Swainson&#39;s hawks, mountain bluebird, red-tailed hawks, prairie falcons, kit foxes, badgers, and chukar.</p><br>
<h2>Protection status</h2><br>
<p>Currently, the 20,400 acres encompassing Conger Mountain are considered a Wilderness Study Area. Action may be taken in the future to designate this area as a National Wilderness Area.</p><br>
<p>Arighi Bianchi is a furniture shop in the town of Macclesfield, Cheshire, England. It was founded in 1854 by Italian immigrants Antonio Arighi and Antonio Bianchi who originated from the village of Casnate on the shores of Lake Como.</p><br>
<p>The shop is recorded in the National Heritage List for England as a designated Grade II* listed building. It has a cast iron and glass frontage, and stands close to Macclesfield Station and Tesco. The four-storey shop front was inspired by Paxton’s Crystal Palace of 1851. It was the work of a local builder George Roylance. The building has much in common with the steel frame buildings of Lower Manhattan. It was saved from demolition in 1973 after a campaign supported by the Victorian Society, the Architectural Review magazine and Sir John Betjeman.</p><br>
<h2>History</h2><br>
<p>Arighi Bianchi (pronounced a-ree-ghee bee-an-key) has been part of the furniture in Britain for over 150 years. It was in 1854 that Antonio Arighi set off from the tiny silk-weaving town of Casnate near Lake Como to escape the ravages of the Italian civil war. After crossing the Alps by toboggan of all things, Antonio A eventually pitched up in Macclesfield, Cheshire. Antonio was soon joined in the town by his nephew Antonio Bianchi and the two men swiftly set up in business as cabinet makers.</p><br>
<p>The 19th century progressed not without incident, with Arighi’s intervention helping to save the town from flooding in 1872 and the decision to move to the current site in 1883. In the early 20th century, the store supplied furniture to Marlborough House and Sandringham House, by royal appointment of Edward VII, Queen Alexandra and Queen Mary.</p><br>
<p>Claise Brook is a stream which empties into Claisebrook Cove before running into the Swan River in Perth, Western Australia. The area surrounding the stream is on the outskirts of the Perth CBD and is part of the suburb of East Perth. Claise Brook was once an important water course from which the numerous interconnected fresh water lakes north of Perth emptied into during the wet season before entering the Swan River.</p><br>
<h2>History</h2><br>
<p>Since the gradual resumption of land over the various feeder lakes, and more recently the East Perth redevelopment in the late 1980s, the stream has become a mainly underground catchment and drainage system and no longer exists as a stream in the normal sense.</p><br>
<p>The stream and cove were initially called Clauses Brook and Clauses Lagoon respectively, however these names appear to have been dropped soon after European settlement: an 1851 newspaper report spoke of the establishment of an abattoir at "Claise Brook". They were named after Frederick Clause who was a naval surgeon that accompanied Captain (later Admiral Sir) James Stirling in their expedition up the Swan River in March 1827. Botanist Charles Fraser who was on the same expedition described the lagoon in his journal:</p><br>
<p>"One mile up the river from the last point is a small creek of fresh water, issuing from an extensive lagoon clothed with arborescent species of Metrosideros of great beauty. The banks are covered with the most interesting plants, amongst which I observed two species of Calytris, a species of Acacia with a scolopendrous-stem, and several Papilionaceous plants. The Angophoras on the flats are gigantic."</p><br>
<p>Since the latter half of the 1800s until the mid-1980s, the area around Claise Brook and Claisebrook Cove was used for mainly industrial purposes and the water quality and surrounds were badly degraded. During this period it was also widely referred to as Claisebrook Drain. In the late 1800s and early 1900s it had become an effluent outlet into the river. In 1906 the Claisebrook and Burswood Sewerage Treatment Works was built. Sewerage was pumped across the river from Claise Brook to ponds and filter beds on Burswood Island.</p><br>
<p>East Perth Gasometer and East Perth Power Station were prominent structures there for many years during the 1900s, both on the northern side of the river outlet.</p><br>
<p>Prior to the redevelopment from the mid-1980s, a major environmental remediation project was undertaken to remove polycyclic aromatic hydrocarbon contaminated soils created by the East Perth Gas Works which operated there from 1922 to 1971. The plant produced gas from coal. Remediation included dredging of six hectares of adjacent riverbeds and removal and treatment of 10,000 m³ of soil.</p><br>
<h2>Redevelopment</h2><br>
<p>The precinct surrounding the Cove is now known as Claisebrook Village and is now mainly residential. The Cove is now a heavily landscaped artificial inlet of the Swan River overlooked by residential buildings and bars, cafes and restaurants. Facilities include moorings and jetties for recreational boating and Trafalgar Bridge which is a pedestrian footbridge which crosses the cove.</p><br>
<p>Crossing the river nearby is Goongoongup Railway Bridge and Windan Bridge which carries road traffic from the Graham Farmer Freeway.</p><br>
<p>The Nakhon Si Thammarat Range  is a mountain range on the Malay peninsula in southern Thailand, running in a north-south direction. This mountain chain is also sometimes named Banthat Range , a name which is however also used to refer to the Chanthaburi mountain range.</p><br>
<h2>Location</h2><br>
<p>The main range of the peninsula begins along the east coast at about 10° 05′ north latitude on Ko Tao. It continues through Ko Pha Ngan and Ko Samui to the east coast mainland, east of Bandon Bay, and parallels the coast all the way into Malayan territory.</p><br>
<h2>Description</h2><br>
<p>The mountains are named after the town Nakhon Si Thammarat, located east of the range. The highest elevation is the 1835 m high Khao Luang.</p><br>
<p>This mountain range is a part of the Tenasserim Hills system. It begins to the east of the Phuket Range, which runs in the same direction about 60 km further west. Between the ranges there are isolated peaks, the highest of which is 1,350 m high Khao Phanom Bencha. To the south it is continued by the Sankalakhiri Range.</p><br>
<p>Several smaller rivers originate in the mountain range, the Tapi River is the largest by far. Another relatively large river is the Trang River.</p><br>
<h2>Protected areas</h2><br>
<p>Several national parks are located in the mountain range.</p><br>
<p>Tai Rom Yen National Park</p><br>
<p>Khao Luang National Park</p><br>
<p>Khao Nan National Park</p><br>
<p>Namtok Yong National Park</p><br>
<p>Khao Pu - Khao Ya National Park</p><br>
<p>Hynds Lodge is a conference and accommodation lodge originally built by Cheyenne, Wyoming businessman Harry P. Hynds and donated to the Boy Scouts of America  in 1922. It is open from May 1 to October 1 by reservation only. It has accommodations for 30 people , a large kitchen, dining room, living room, covered porch, stone fireplace and chimney, and 9 acre of land. The lodge was originally used by Wyoming Boy Scouts as a recreational camp. Later it was used by churches, social groups, and businesses. It was built on land that became part of Curt Gowdy State Park in 1971 and is now operated by the park. The south fork of Crow Creek lies nearby, with a granite outcrop and woodlands of cedar and spruce.</p><br>
<p>The lodge has many large trees around it, towering granite behind it, and is built into a hillside. Its construction with granite stone in ashlar masonry gives it a unique architectural style. The University of Wyoming&#39;s Department of Geology and Geophysics offers summer field courses in the area of the park and stays at the lodge. The lodge was added to the National Register of Historic Places on March 23, 1984.</p><br>
<p>Hynds arrived in Cheyenne in 1882 from Illinois. He began working as a blacksmith but in 1883 he acquired the first of several gambling saloons. This made him quite wealthy and he entered other businesses and also became an philanthropist. He was a founder of Frontier Days Rodeo. The Boy Scouts of America was very popular in Cheyenne by 1922 and their leadership approached him to help raise money for a cabin. Instead, Hynds paid for the cabin himself. The cabin was completed in the summer of 1922 and measures 36 x 35. The lodge was operated by the Young Men&#39;s Literary Club for the Boy Scouts until 1935, when the City of Cheyenne took over. Many civic organizations have used it since, including the Boy Scouts. Major repair efforts were made in 1966. In 1971, the lodge and its land were leased to the Wyoming Recreation Commission by the City of Cheyenne.</p><br>
<p>Desatoya Peak is the tallest mountain in both the Desatoya Mountains and Churchill County, in Nevada, United States. It ranks forty-third among the most topographically prominent peaks in the state. The mountain has two peaks with the south peak being the tallest at 9,977 ft while the north peak has an elevation of 9,970 ft. It is located about 38 mi west of Austin and 55 mi east of Fallon, along the boundary between Churchill County and Lander County. The peak is on public land administered by the Bureau of Land Management and thus has no access restrictions.</p><br>
<h2>Conservation</h2><br>
<p>The 51,402 acre surrounding Desatoya Peak are part of the Desatoya Mountains Wilderness Study Area which is administered by the Bureau of Land Management. Wildlife that make their home here are mountain lion, mule deer, gray fox, sage grouse, red-tailed hawk, golden eagle and pika. Additionally, brook trout and Humboldt cutthroat trout live in some of the permanent streams on the flanks of Desatoya Peak.</p><br>
<p>The Granada Theater, located on 2nd and Washington streets in The Dalles, Oregon, United States, was built in 1929. The exterior of theater is in the Moorish Revival style.</p><br>
<p>This theater is said to have been the first theater west of the Mississippi to show a "talkie".</p><br>
<p>A plaque bearing the seal of the State of Oregon on the side of the building reads, "Granada Theater: This Moorish-style motion picture theater was completed in 1930 for its first proprietor, M.R. Matthew, at a cost of $125,000. The plans were prepared by William Cutts of Portland, who designed approximately sixty theaters for the Universal Film Corporation. Planned at the height of the silent screen era, the theater nonetheless was equipped with Vitaphone and Movietone sound systems. The facade of the concrete building was detailed to imitate Moorish Architecture. Its stucco finish was accented with brick and tile, and its domed towers, arcaded parapet, and horseshoe-arched windows framed by twisted spiral columns were designed to create the exotic atmosphere of the Mediterranean."</p><br>
<p>The City of The Dalles purchased the theater in September 2010.</p><br>
<p>Van Salsbergen House, also known as the Black House and Van Hoesen Stone House, is a historic home located in Greenport near the city of Hudson in Columbia County, New York. It was built about 1700, and is a 1 1/2-story stone dwelling with a steeply pitched gable roof. Originally two-rooms large, it was expanded about 1860 with the addition of the north room. As its name implies, the house derives from the original owner and builder, Jan Hendricksen Van Salsbergen, an early settler of the area. He was known to have been born in the Netherlands in the 17th century and died in Columbia County in 1710 as per available records. It is currently undergoing restoration by its private owner. The structure is unique by reason of its scissors- truss design being infrequently employed in the geographical area but typical of housing design seen in the Netherlands.</p><br>
<p>It was added to the National Register of Historic Places in 2010.</p><br>
<p>The United States Post Office in downtown Crawford, Nebraska is a historic edifice built to house the Crawford branch of the United States Postal Service. It was built in 1938-1939 and was added to the National Register of Historic Places on May 11, 1992, as part of the Nebraska Post Offices Which Contain Section Artwork MPS.</p><br>
<h2>Description</h2><br>
<p>The Crawford US Post Office is located at the northwest corner on 2nd and Main Streets in the commercial district of Crawford, Nebraska. It was built in the Moderne style in the late 1930s from standardized blueprints. Included in the listing are three contributing objects: two ornamental lampposts flanking the staircase to the main entrance and a flagpole. The structure has one story with a basement and measures approximately 60 by. It is constructed of red brick with a concrete base and topped by a limestone parapet. The main entrance features an aluminum grill with a stylized eagle above the doorway. Two recessed windows with limestone sills are located on each side of the entrance. Although they were originally triple-hung, the upper thirds have been filled in with wooden panels. The architectural features of the front facade are echoed on the remaining sides of the structure. A handicap ramp has been added on the structure&#39;s west side, and an enclosed stairwell on the east side provides access to the basement.</p><br>
<p>Inside, the lobby features original marble floors and wainscoting, radiators, and woodwork. The space immediately inside the front entrance is surrounded by a vestibule that projects into the lobby. The building&#39;s original light fixtures have been replaced since the original construction, as have the front doors.</p><br>
<p>The lobby&#39;s most prominent feature is a mural on the upper portion of the east wall. It was painted by G. Glenn Newell, an artist and dairy farmer from Dutchess County, New York, and installed by post office workers in May 1940. The piece depicts a wagon train beginning to ford a stream. The lead wagon dominates the scene with other wagons visible in the background, along with local landmark Crow Butte.</p><br>
<h2>History</h2><br>
<p>The first area post office was established in June 1884. It was located four and one-half miles (about seven kilometers) south of what is now Crawford, and was known as the Crow Butte/Sioux County branch. After Dawes County was formed from the western portion of Sioux County, the post offices name and site changed to Crawford. It became a second-class branch on July 1, 1912. City delivery was established on July 1, 1930. After being located in many different locations in town, it moved to the current building, which was built in 1938-1939 and dedicated during the communitys 1939 Labor Day celebration.</p><br>
<p>The edifice&#39;s mural, titled "The Crossing" and painted by G. Glenn Newell, was one of hundreds commissioned by the Section of Fine Arts in the late 1930s and early 1940s. Newell received a notice from the section inviting him to submit designs for the Crawford Post Office in August 1939. Newell immediately accepted the commission, for which he would be paid $800. Although he did not visit Crawford before painting the mural, he received several photographs from the Crawford postmaster to aid him in accurately painting the setting. Newell originally conceived the idea of including a poem with the mural, which read, "Seeking the westward sunshine/ Leaving storms behind/ Taking sires of the future with them/ And dams of a better kind." He was informed this was unnecessary. The completed mural was shipped to Crawford in April 1940. It was professionally cleaned and restored in 1981.</p><br>
<p>The Crawford postmasters have included John Walsh, Cyrus Fairchild, Lee Van Voorhis, C.W. Fritts, George C. Scott, John Pat Davis, John Lemons, Edwin Gorton, Frank Reeves, and Mary Jo Knoell.</p><br>
<p>Nagle Warren Mansion, also known as Cheyenne YWCA Building, is former residence and YWCA with three buildings located in Cheyenne, Laramie County, Wyoming. It is now a bed and breakfast  establishment with 12 guest rooms decorated in Victorian West style. One guest room is a suite and each room has its own bath. Six rooms are in the main house and six in the carriage house. There are three conference rooms. The B&B has a AAA 4 diamond rating. Furnishings are authentic to the period of the American Old West and include: furniture, wallpaper, brass marble, bronze or gas fireplaces, ornate staircases, woodwork of cherry, mahogany, and oak, and stained glass windows. There is some Moorish tile and a Moroccan chandelier.</p><br>
<p>The mansion was built as a residence in 1888 by Erasmus Nagle. It is one of the few homes from the 1800s left standing in Cheyenne. The Senator died in 1929 and Clara gave the mansion to the YWCA. In 1960 the soft outer stone, which had been predicted back in 1880 to be too soft, began to crumble and the exterior was covered in stucco. Don and Barbara Sullivan began living there with their children in 1985 when they bought the house. Jim Osterfoss bought it in 1997, restored it, and turned it into a B&B. There is also a stone carriage house which was originally a stable for four horses. The stable house was later used as an automobile garage and during the YWCA years as an entertainment center. The original stone smokehouse is still standing, making a total of three buildings on the property. The carriage and main house are now connected. The house was added to the National Register of Historic Places on July 12, 1976.</p><br>
<p>The Negri River is a river in Australia. It flows from the Northern Territory into Western Australia, where it merges with the Ord River to become part of the Ord River catchment. It is roughly 100 kilometres long.</p><br>
<p>It was named by Alexander Forrest on 2 August 1879, the same day he named the Ord River. The following is from his journal.</p><br>
<p>We started on again today, and steering N. E. and E.N.E. for about six miles, we came to a large river, very similar in character to the one we have been following down during the last week. I have named this river the Negri, after Commander Christopher Negri of Turin. In all probability it joins the one we have just left; so, after crossing it, we turned Northwards, hoping again to come upon the larger stream.</p><br>
<h2>Environment</h2><br>
<p>Many parts of the river&#39;s catchment suffered erosion and become degraded due to overgrazing in the first half of the 20th century. The increased sediment load posed a long-term threat to the Ord River Dam that required a regeneration project which began in 1960.</p><br>
<p>The 1907 Dorris Motor Car Company Building is a factory and industrial warehouse located at what is now 4059 – 4065 Forest Park Avenue in the Central West End neighborhood of St. Louis, Missouri. The building was originally constructed in 1907 as an automobile factory for the Dorris Motor Car Company and was modified in 1909 with the addition of a third story. It was the headquarters and manufacturing facility for the company until 1926, and the company played a significant role in the establishment of St. Louis as an automotive assembly and parts manufacturing center. It was listed on the National Register of Historic Places on February 10, 2000.</p><br>
<p>In 1926, the Dorris Motor Car Company officially went out of business, but the building has seen subsequent use. It held the Brauer Brothers Manufacturing Company&#39;s shoe factory for many years. After the Brauer Brothers Manufacturing Company moved out, the space was used for retail purposes by a furniture store. It then sat vacant for years. In 2004, it was renovated for use by the Center for Emerging Technologies, a startup incubator that is now called the CIC@CET. The building is undergoing further renovation today for continued use by the CIC@CET.</p><br>
<p>The Simeon Rockefeller House, also known as Rockefeller Tavern, is a historic house located in Germantown, New York.</p><br>
<p>The beginnings of the noted family in American history can be traced to this historic home. As indicated on the historical marker placed by the State of New York, it was the home Simeon or Simon Rockefeller (1730-1795), son of the immigrant Diell Rockefeller. This family originated among the Palatine Germans who immigrated to Columbia County seeking religious freedom. Descendants include John D. Rockefeller who was known to have visited the site. It was added to the National Register of Historic Places in 2009. While it is now undergoing restoration as a private residence, it was originally a stage stop, tavern, and restaurant. In addition, the early settlers engaged in farming. It is a plain structure with colonnades on a double porch. It is built with fieldstone and as was typical, had a basement kitchen.</p><br>
<p>The house was in poor condition and had had many unsympathetic alterations when it was bought by Mary Black and Michael J. Blackstone. The two friends restored the building and used it as separate but conjoined residences; the central hall was agreed upon as the dividing line, and both agreed to give the other veto power over any exterior alterations.</p><br>
<p>Kluge House, also known as Maverick House, is a rare example of Silesian fachwerk, log and half-timber construction, located in Helena, Montana. In mid-1964 the home was almost destroyed as a fire hazard as it had fallen into disrepair and transients were living in it. A shed is attached to the north side of the house. The second floor was built in 1882. Prior to that Kluge had apparently done significant work on the original cabins first floor, which has hewn squared logs. The second floor is half-timber filled in with bricks. The second floor diagonal logs brace the framing logs. The overall dimensions of the house are 30-11" x 16&#39;-4" with a foundation of stone found locally. There are front and rear doors on the first floor. The front door is asymmetrically located and the rear door is near a corner. The second floor is reached only via an exterior staircase. The house has a brick fireplace. The first floor has an entrance vestibule and two rooms of dissimilar size. The smaller room has a hatch leading to a cellar. The second floor has a floor plan that is very similar to that of the first floor but it is reversed, i.e., two rooms and a vestibule. Floors are wooden.</p><br>
<p>Emil Kluge was born March 28, 1845 in Prussia. Kluge served in the infantry, in both the Austro-Prussian War in 1866 and the Franco-Prussian War in 1870, in the latter of which he was wounded. Kluge and his family came to America from Germany in 1871, first settling in Detroit, Michigan for two years, and then Helena, Montana, arriving on May 3, 1873. At that time, the family moved into this house, which was an abandoned miners cabin. Kluge worked mostly as a contractor, but also as a gold prospector, constable, and Justice of the Peace. He was an officer in one of Helenas Masonic lodges and was a member of the Odd Fellows. Kluge resided in Helena until his death, September 26, 1924.</p><br>
<p>The Hansel Mountains are a 35 mi long mountain range located in north Utah on the northern border of the Great Salt Lake.</p><br>
<p>Located in northeast Box Elder County, the southwest of the range abuts the Locomotive Springs State Wildlife Management Area; the northeast end of the range ends at a lower elevation divide between the North Hansel Mountains that lie on the Utah-Idaho border. Snowville lies on Deep Creek in the Sage Valley to the northwest. Interstate 84 travels northwest-southeast through the mountain divide. The mountain range continues southwest and south and ends at Monument Point overlooking the Great Salt Lake to the south, and the wildlife management area to the west.</p><br>
<h2>Peaks</h2><br>
<p>The highest elevation in the mountains is an unnamed peak 6,243 ft on the southeast ridge of the range. Monument Peak, 5,997 ft, is located at the southwest end of the range.</p><br>
<p>The Curlew Valley is a 23 mi long valley located on the northern edge of the Great Salt Lake in Box Elder County in northern Utah and extending north into Oneida County in southern Idaho.</p><br>
<p>Within northeast Box Elder County, the southwest of the valley abuts the Locomotive Springs Wildlife Management Area and an extensive salt flat on the edge of the Great Salt Lake.</p><br>
<h2>Description</h2><br>
<p>The Curlew Valley trends southwest to northeast with Deep Creek towards the valleys west. At the valleys northeast, Deep Creek turns east, then almost due north into Idaho, meeting the unincorporated community of Stone and the south border of the Curlew National Grassland. Adjacent to Stone, upstream and south is the townsite of Snowville, Utah on Interstate 84 which traverses the valley diagonally from northwest (Idaho), by southeast. The route goes through the divide between the Hansel Mountains (south), and the North Hansel Mountains and continues southeast through the Blue Creek Valley, the south West Hills and continues on to Brigham City.</p><br>
<p>The Curlew Valley center is slightly east-southeast of Coyote Springs, on Deep Creek. A mountain peak, Cedar Hill lies adjacent eastwards, 5,181 ft. Directly west, and south of Coyote Springs lies another peak, Wildcat Hills, 5,077 ft.</p><br>
<h3>Rose Ranch Reservoir</h3><br>
<p>At the northeast of the valley, the Stone Hills force Deep Creek to transect east; here, about 3 - west and southwest of Snowville is the Rose Ranch Reservoir, formed on Deep Creek.</p><br>
<h2>History</h2><br>
<p>Curlew Valley, named after the curlew snipe that nests there. The first recorded white men were Peter Skene Ogden&#39;s large party of trappers that camped on Deep Creek December 27, 1828.</p><br>
<p>Some of the discharged members of the Mormon Battalion, on their way home from California to Salt Lake City on September 18, 1848, camped on Deep Creek and also in a cave 1 mi east called Hollow Rock.</p><br>
<p>The beginning of Deep Creek is a large spring at Holbrook which runs through the center of the valley and has never varied even in dry years. About 1 mi southwest is Rocky Ford, where the pioneers were able to pass on solid rock.</p><br>
<p>In 1869 William Robbins, Thomas Showell, and William M. Harris settled at the Curlew Sinks, 10 mi west of here, where Deep Creek sinks into the ground. The old pioneer trail and the stage line went through their ranch.</p><br>
<p>The first townsite in the Curlew Valley was Snowville. Settled at the direction of Brigham Young and named in honor of Lorenzo Snow: an apostle at the time, but later to become the 5th President of The Church of Jesus Christ of Latter-day Saints 1898–1901. Snowville was laid out August 14, 1878.</p><br>
<p>The Wick Building, also known as The Wick Tower, is a high rise structure and second tallest building in Youngstown, Ohio. Constructed by D. H. Burnham & Company in 1910, the structure contains 13 floors and rises to a height of 184 feet. It is a classic example of Chicago School architecture, and contains a row of arches at the crown. The Wick Building was the tallest building in the city until the construction of Metropolitan Tower in 1929. It was listed on the National Register of Historic Places on February 8, 1980.</p><br>
<h2>Redevelopment</h2><br>
<p>The NYO Property Group bought the Wick Building in 2012 with plans of redeveloping the building into apartments. In August 2015, the building was reopened as The Wick Tower, a mix of apartments and extended stay properties, with commercial space on the first floor.</p><br>
<h2>Further reading</h2><br>
<p>Chacana is a large 32-km long - 18-24 km wide caldera that has erupted in historical times. It forms one of the largest rhyolite centers in the Northern Andes with major eruptions over the past 240,000, 180,00, and 160,000 years ago and has had andesitic-rhyolitic volcanism. With dactic lava flows continuing into historical times. Lava domes were also constructed in the Holocene. Chacana is located 30 km from Quito and the large Antisana volcano is constructed to the southeast.</p><br>
<h2>Eruptions</h2><br>
<p>Eruptions in the past 10,000 years have been limited to small lava flows originating from Fissures.</p><br>
<p>1760 Eruption: A small (VEI 0) Eruption, the first in historical time, came from a flank vent on the SW of the Caldera which caused some damage.</p><br>
<p>1773 Eruption: Another small eruption took place in 1773. It came from a fissure in the South part of the caldera.</p><br>
