<p>Onancock Historic District is a national historic district located at Onancock, Accomack County, Virginia. The district encompasses 267 contributing buildings, 2 contributing sites, and 2 contributing objects. It includes most of the historic residential, commercial, and ecclesiastical buildings in the town of Onancock. The buildings represent a variety of popular architectural styles including the Late Victorian, Greek Revival, and Federal styles. Notable buildings include Scott Hall , Alicia Hopkins House , Harmon House , Holly House , Ingleside , Dr. Lewis Harmanson House , Harbor Breeze , First National Bank , Roseland Theatre , Market Street Methodist Church , Naomi Makemie Presbyterian Church , the Charles E. Cassell designed Holy Trinity Episcopal Church , Onancock Town Hall , Onancock High School , and Onancock Post Office . Located in the district and separately listed are the Cokesbury Church, Hopkins and Brother Store and Kerr Place.</p><br>
<p>It was added to the National Register of Historic Places in 1992.</p><br>
<p>Gartz Court is a bungalow court located at 745 N. Pasadena Ave. in Pasadena, California. The court consists of five buildings containing six residential units, which surround an oval rose garden and walkways. Built in 1910, the court, along with Bowen Court, is one of the oldest remaining in Pasadena. The court was commissioned by Kate Crane Gartz, the heir to Crane Plumbing, and was designed by Myron Hunt and Elmer Grey. The homes&#39; designs were influenced by the English Arts and Crafts Movement and feature stone chimneys, wood shingled skirts, and Tudor Revival-style half-timbering. The court was originally located at 270 N. Madison Ave., but was moved to its current location in 1984 to save it from demolition.</p><br>
<p>The court was added to the National Register of Historic Places on August 25, 1983.</p><br>
<p>Building 98 at Fort D. A. Russell is the historic US army base bachelor officer quarters, officers club, and grand ballroom near Marfa, Texas; it was active from 1911 to 1946. Building 98 is Located at Fort David A. Russell&#39;s central fort complex. It is a project of the International Woman’s Foundation and it is the home of the World War II German prisoners of war POW murals.</p><br>
<h2>Murals</h2><br>
<p>The murals were painted in the state dining room and in the base library. Encompassing over 3,048 square feet of wall space, making them a unique historic national treasure. The Murals were completed in 1945 by Hans Jürgen Press and Robert Humpel, both German prisoners of war held at the base. The artist and writer Hans Jürgen Press was a sail plain glider pilot based in France during the war, and departed building 98 in 1945; While there he created two west Texas watercolors of local residents — one performing a Spanish dance and another playing the Spanish guitar. Building 98 stands as a testimony to Marfa&#39;s long standing history in the arts. West Texas regionalism has a history in Texas dating back to the cattle drive of which Marfa had many.</p><br>
<h2>History</h2><br>
<p>In 1911 the United States Cavalry occupied the building where it served as the Bachelor Officer Quarters (BOQ) and as an entertainment center for West point Officers during World War I and the Mexican Revolution. The fort was established to protect local ranches and town citizens during dangerous times along the Texas and Mexico border. Building 98 also faced the main fort parade grounds and was the location of the original camp Alberts command headquarters. Also housed at Building 98 was the fort officers mess which had a full-time chef and large dining room. Building 98 also features a World War II ASM-N-2 BAT Glide Bomb cart from the original air base.</p><br>
<p>In 1949, the historic base was sold to J. Alfred Roosevelt. The International Woman&#39;s Foundation was responsible for placing Fort D. A. Russell on the National Register of Historic Places and for listing the base at the Texas Historical Commission, a long time dream of Roosevelt who had lived at the complex.</p><br>
<p>The International Woman&#39;s Foundation has operated an artist in residency program and Camp Marfa fort museum since 2002. In 2002 Mona Blocker Garcia took on the task of creating the foundation for mature woman artists and healthful aging thus preserving the important history of Fort D. A. Russell to its exact state when the fort closed. The George Sugarman courtyard is a permanent installation highlighted at the Building 98 metal sculpture garden</p><br>
<h2>Renovations</h2><br>
<p>The International Woman’s Foundation has been authentically restoring the building to its original integrity and is responsible for Fort D. A. Russell being placed on the National Register of Historic Places and the Texas state historical society register of historic places. Major renovations began in 2002 with the complete replacement of the structures roof and outside integrity of the walls. Imphasis on floors, furnishings and ceilings are maintained with original features negating intrusive damages caused from modernization after 1949. The building also had serious damage that occurred after the great depression. Today the restored Building 98 museum is open to the public and a guided tour is available. Building 98 is one of Marfa&#39;s most important historic places with a rich history that has been brought back to life within its unique complex. Preserving the history of the original army camp for future generations allows Building 98 stand as an important resource to understand and appreciate the significant roles Texas has played during times past.</p><br>
<h2>Art galleries</h2><br>
<p>Building 98 requires an artist in residence to exhibit their works and the foundation provides the Studio 98 galleries as a venue and hosts a reception in the historic officers club. Events are yearly and are published through media agencies by advertisement. Important exhibitions include a major retrospective of the works of Wilhelmina Weber Furlong in the grand ballroom featuring over 75 unseen works of the early American modernist. An exhibit of the private belongings of the artist was displayed including her Victorian easel. The event served as the ten year anniversary gala for the foundation in October 2012</p><br>
<p>Las Casitas Court is a bungalow court located at 656 N. Summit Ave. in Pasadena, California. The court, which was built in 1916, consists of ten buildings containing twelve residential units and arranged in two rows; the rows of homes flank a narrow courtyard with two walking paths. The homes in the court were designed in the American Craftsman style, and the court is one of the few surviving Craftsman-styled courts. The first four houses from the street in each row feature gable roofs with wide eaves and porches with shed roofs, while the last two houses have pergolas over their entries. The courtyard includes a torii and decorative boulders.</p><br>
<p>The court was added to the National Register of Historic Places on July 11, 1983.</p><br>
<p>The Russian Bishops House, once the Russian Mission Orphanage, is a historic house museum and National Historic Landmark at Lincoln and Monastery Streets in Sitka, Alaska. Built in 1841-43, this log structure is one of the oldest surviving buildings of Russian America, and was one of the centerpieces of the Russian Orthodox churchs efforts to spread its influence among the natives of Alaska. It was the home and administrative center of Ivan Veniaminov, the first Bishop of Alaska, later canonized as Innocent of Alaska. The house is now a unit of Sitka National Historical Park, and is administered by the National Park Service.</p><br>
<h2>Description</h2><br>
<p>The Russian Bishop&#39;s House is a two-story log structure, measuring about 42 x. It is divided into nine bays, each measuring about 7 ft (one sazhen) square, and covered by a hip roof. The east and west ends of the building are further extended by shed-roof "galleries" that are 14 ft wide, which historically provided space for stairwells, storage, latrines, and entrances.</p><br>
<p>The exterior has undergone a number of alterations since construction. The south facade was sheathed in clapboarding c. 1851, and the galleries were roofed in metal around that time. In 1887 the galleries were sheathed in board-and-batten siding. The interior was repeatedly altered over the decades, and underwent a major restoration once the property was acquired by the National Park Service 1973.</p><br>
<h3>Secondary buildings</h3><br>
<p>The property on which the Bishops House stands includes two secondary buildings associated with the activities of the Russian Orthodox Church. East of the main house stands the Old School, a two-story wood frame structure built in 1897 to provide a kindergarten and girls school. House 105 is a 1-1/2 story wood frame structure which stands facing Monastery Street. It was originally on a separate parcel of land, and was apparently moved to its present location in the 1950s.</p><br>
<h2>History</h2><br>
<p>The Russian Bishops House was built between 1841 and 1843 by Finnish laborers brought in by the Russian American Company, to provide housing for Reverend Ivan Veniaminov, who had been appointed the first Bishop of Alaska by the Russian Orthodox Church. From his seat in Sitka, Veniaminov oversaw the spread of Orthodox missionary and educational work to the indigenous peoples of southern Alaska, nearly doubling the number of Orthodox worshippers in the region between 1841 and 1860. Missionary efforts were continued after the United States purchased Alaska in 1867, and were only significantly cut back after funding cuts in the wake of the Russian Revolution in 1917. The seat of the Russian diocese was relocated the San Francisco in 1872, and the Bishops House was repurposed to provide housing quarters for priests. Its first floor also served as an inn for a time.</p><br>
<p>In 1903 a bishop was once again assigned to a district with its seat at Sitka. For most of the 20th century, the upper floors house a chapel and the quarters of the bishop, while the ground floor was used in a variety of ways. In the 1920s it housed a printing operation that produced, in addition to church publications, the Sitka Sun and the Sitka Tribune.</p><br>
<p>The Old School was used as a church school building until 1922, and as a public school thereafter. House 105, while not of architectural note, was used as a church rental property for many years, and is one of the oldest buildings in Sitka.</p><br>
<p>The property was designated a National Historic Landmark in 1962, and was listed on the National Register of Historic Places as the "Russian Mission Orphanage" in 1966, reflecting its major function at that time. The National Register designation was altered to "Russian Bishop&#39;s House" in 1980.</p><br>
<p>The Russian Bishop&#39;s House is now owned and managed by the National Park Service as a unit of Sitka National Historical Park. It is open to the public on ranger-guided tours.</p><br>
<p>Manipa Island is an island in West Seram Regency, Maluku Province, Indonesia. It is located 8 km off the western coast of Kelang at the western end of Seram Island and 25 km off the western coast of Buru. The inhabitants speak the Manipa language, as well as Indonesian and Ambonese Malay.</p><br>
<p>This island gives its name to the Manipa Strait between Buru and Seram.</p><br>
<h2>Adjacent islands</h2><br>
<p>Manipa has a number of small islands that are very close to its shores.</p><br>
<p>Masawi and Asamamonuke on a reef on its northeastern coast.</p><br>
<p>Suanggi off its western tip. It is located in the Manipa Strait between Buru and Seram. 3&deg;18&prime;S latitude, 127&deg;28&prime;E longitude</p><br>
<p>Tuban in the south</p><br>
<p>Luhu in the north.</p><br>
<p>The Schuetz Log Cabin, near Dalton, Nebraska, is a historic log cabin that was listed on the National Register of Historic Places in 2011.</p><br>
<p>It was built sometime between 1900 and 1920 and was deemed significant in the local area "for architecture as an excellent example of log construction in Morrill County, Nebraska." As of its NRHP nomination date in 2011, the cabin was in "fair" condition and "its core character defining features" were being revealed in rehabilitation in progress.</p><br>
<p>It was built on the homestead of Louie Schuetz, who claimed 160 acre of land under the Homestead Act in 1890, after finding the site while hunting. Its attraction was that it had water. His property grew to 880 acre and his wife, Margaret Jane Hughes, had 160 acres more. After they married in 1891, they built and lived in, in succession, a sod house, then a native stone house, then the surviving log cabin, and later a frame house.</p><br>
<p>The Lloyd M. Joshel House, also known simply as the Joshel House, is a private residence in the Hilltop Neighborhood of Denver, Colorado. Built in 1951, it is known as one of the finest examples of the International Style in residential architecture in Denver. The property is a local City of Denver Landmark and is listed in the National Register of Historic Places.</p><br>
<h2>International Style</h2><br>
<p>The Joshel House is a distinctive example of the International Style. The International Style emphasizes the expression of volume rather than mass, balance rather than symmetry, and the absence of ornament. The philosophy underpinning the International Style also promotes, among other things, logical design to support building function and truth to materials. The International Style is rare in residential buildings in Denver, although contemporary commercial examples, including I.M Pei’s Mile High Center, are not uncommon. The International Style contrasts with Usonian and modern expressionist examples more common in the greater Denver area.</p><br>
<p>The nomination form for inclusion in the National Register of Historic Places describes the architecture of the house:</p><br>
<p>The house was designed by the husband and wife architecture team of Joseph and Louise Marlow, who designed numerous mid-20th Century structures, including the Far View Visitor&#39;s Center at Mesa Verde National Park.</p><br>
<h2>Lloyd and Suzanne Joshel</h2><br>
<p>Lloyd M. Joshel and Suzanne Joshel reflected in their lives the changing cultural and social landscape of post World War II era in the United States. Mr. Joshel was a prominent figure in Colorados Cold War history. Mr. Joshel was born in Geneva, Ill. in 1914 and died in Denver in 1999 at the age of 84. Educated at the University of Illinois and University of Ohio, and at Harvard University, Mr. Joshel was a chemist before and during World War II and, later, a business executive. He became the general manager of Dow Chemicals Rocky Flats nuclear weapons plant in 1964. Mr. Joshel was general manager during a major fire that caused significant damage and contamination to the Rocky Flats facility.</p><br>
<p>Suzanne Joshel was a noted Denver patron of the arts. Ms. Joshel was born in 1921 in Berlin and after attending a year of college in Germany, her family sent her to London to escape the Nazis. Ms. Joshel met Lloyd Joshel in the United States and married him in 1947. They were divorced in 1994. Ms. Joshel was active in numerous causes, including helping pass the Voting Rights Act, and she was president of the Colorado League of Women Voters. Ms. Joshel amassed a large art collection, and the gardens at the Joshel House were dotted with many sculptures collected by her. Ms. Joshel died in 2009.</p><br>
<h2>Historic Designation</h2><br>
<p>The Joshel House was nominated for inclusion on the National Register of Historic Places and was officially entered into the register in on December 28, 1995. The nomination form described the significance of the house as “the best example of a post World War II International Style residence in Denver.” At the time of its entry into the register, it was one of only a very few post World War II residences considered eligible for the National Register.</p><br>
<p>The Joshel House was designated as a City of Denver Landmark on November 10, 1994.</p><br>
<p>Sgùrr na h-Ulaidh   is a mountain lying to the south of the village of Glencoe in the Scottish Highlands. The mountain cannot be seen from the main A82 road as it is hidden behind Aonach Dubh a&#39;Ghlinne.</p><br>
<h2>Ascent</h2><br>
<p>The usual route of ascent is from Glen Coe, approximately 2 km west of Loch Achtriochtan. A track on the west of Allt na Muidhe is followed and after 1 km the burn is crossed. The east side of the burn is then followed for about 3 km until a turn east is made to climb to the ridge just north of the top of Stob an Fhuarain. This peak is climbed, then the steep, rocky ridge is followed trending south-west to the summit of Sgùrr na h-Ulaidh.</p><br>
<p>A route that avoids the steep ground on the north side of the mountain can be made from the southern Glen Etive side.</p><br>
<p>The Cannonball House located in Macon, Georgia, United States was constructed in 1853. The house was named the Cannonball House because of cannonball-inflicted damage sustained during the Civil War. The house was built using an authentic Greek revival architectural style and is listed in the National Register of Historic Places.</p><br>
<p>The recreated meeting rooms of the Adelphean (ΑΔΙΙ) and Philomathean (ΦΜ) societies (the world&#39;s first sororities established at Wesleyan College in 1851 and 1852) can be found on display inside the house. The entire house is furnished to the 1853 period.</p><br>
<p>The rear of the Cannonball House is occupied by a two-story kitchen built of hand-molded brick. The upper level of this house formerly served as servants&#39; quarters. Few structures of this type remain in the South today. A bronze cannon, forged in 1864 at the Macon Arsenal, can be found on display in front of the Cannonball House.</p><br>
<h2>History</h2><br>
<p>The house received its name due to a Union cannonball that crashed into it during the Battle of Dunlap Hill on July 30, 1864.</p><br>
<p>The left middle column of the house was destroyed by a cannonball fired from across the Ocmulgee River. According to eyewitnesses, the cannonball went through the column and into the house itself after bouncing off the sand sidewalk in front of the house. Evidence of the impact still remains today and can be seen in the repaired column, parlor plaster and large dent in the hall floor.</p><br>
<p>The Cannonball House was owned by Judge Asa Holt during the war. The house is now owned by the Sidney Lanier Chapter of the United Daughters of the Confederacy (UDC).</p><br>
<p>Currently, the house serves as a historic house museum.</p><br>
<p>Captain Timothy Hill House is a historic home located at Chincoteague Island, Accomack County, Virginia. It was built about 1800, and moved to its present location in 1980 when faced with demolition. It is a 1 1/2-story dwelling that was built using pit sawn and hewn pine planks and measures 17 feet, 4 inches, by 16 feet, 4 inches. It currently sits on a low brick pier foundation. It has a modern roof featuring a steep side gable with wood shingles and weatherboard. The house has a wooden chimney that represents the first period of this house and features carvings of sailing ships of the period on the exterior</p><br>
<p>log walls. It is significant as a rare surviving example of log plank construction still existent in Virginia, possibly the oldest remaining house on Chincoteague Island, and one of the few houses remaining in Virginia which at one time had a wood chimney.</p><br>
<p>It was added to the National Register of Historic Places in 2011.</p><br>
<p>The USA Post Office, also known as the Willows Main Post Office or US Post Office&ndash;Willows Main, is the main post office in Willows, California. Built in 1918, the post office was designed by Walter D. Bliss and William B. Faville, architects known for their work in San Francisco. The building was designed in the Italianate and Beaux-Arts styles. The building&#39;s roofline and arched arcade entrance with Doric columns were inspired by the Italianate style, while its detail work, including terra cotta reliefs, quoining, and decorative keystones, is Beaux-Arts styled. While many Italianate Beaux-Arts post offices were built in the early 20th century, the Willows post office was one of the few built in California. In addition, it is one of the few ornately designed buildings in Willows and has been called the "most sophisticated and imposing" of those which exist.</p><br>
<p>The post office was added to the National Register of Historic Places on January 11, 1985.</p><br>
<p>Lake Howard is a fresh water lake, located in Winter Haven, Florida. The lake is part of the headwaters of the Peace River watershed. Lake Howard is a prominent lake in Winter Haven&#39;s Chain of Lakes. Lake Howard is on the southern chain of lakes. It is connected to Lake Cannon, to the north-west, and Lake May, to the south-east. Lake Howard has a surface area of 624 acres. It has a mean depth of 10.9 ft, and maximum depth of 18.7 ft.</p><br>
<p>The Calusa were the first known people to live along this lake. The Seminole were later known to live and hunt along the lake. Lake Howard was first surveyed by Dr. John Westcott in 1849. He named the lake for his neighbors in Madison County, Florida, the Howard family. The lake, with its current name, appears in the first United States government maps of the area, published in 1854.</p><br>
<p>Lake Howard became one of the first areas to be settled by newly arriving American and European settlers. Some of the oldest homes in the city of Winter Haven are located on the shores of Lake Howard. Beymer Memorial United Methodist Church, located on the north-east side of the lake, is one of the oldest buildings in Winter Haven. On the north side of Lake Howard is the residential neighborhood of Interlaken. This neighborhood is a designated USA Historic District, with over 50 homes on the National Register of Historic Places.</p><br>
<p>By the late 1960s, Lake Howard started to become polluted. The single biggest problem was that over-flow capacity lines for the Jan Phyll Village Waste Water Treatment Facility, which fed directly into Lake Howard. This meant that raw sewage was periodically sent directly into the lake. This problem was corrected in 1977, when the waste facility was re-designed. In 1980, an important restoration study was done on Lake Howard to improve the water quality. Over the preceding years, many other major scientific studies were conducted on Lake Howard, often building upon work done in previous studies. In 1995, Dr T.J. Whitmore conducted a major paleolimnological study on Lake Howard. By examining sediment core samples, he was able to evaluate historical changes in water levels and water quality in Lake Howard. Today, through conservation and restoration efforts, by the city, state, and federal government, the water quality of Lake Howard continues to improve. However, rapid urbanization around the lake threatens its future health.</p><br>
<p>Lake Howard is situated relatively close to the downtown area of Winter Haven. Lake Howard Drive, which circles the lake, is a busy thoroughfare in the city. The lake is surrounded by both residential and commercial properties. There are two public boats ramps which can be used to access the lake. The Lake Howard Boat Ramp West is located at the corner of Lake Howard Drive and Avenue B NW, and has a boat ramp and a fishing pier. Lake Howard Boat Ramp East is located at the corner of Lake Howard Drive and West Central Avenue, and has a boat ramp, fishing pier, parking area, and picnic area.</p><br>
<p>South Lake Howard Nature Park is located on the south-west side of Lake Howard. The park is an important role in the restoration of the ecology and water quality of Lake Howard. It is also plays an important role in the reclamation of natural wetlands within the city of Winter Haven. The park has multi-use trails, picnic areas, and restrooms. The park also has a wooden boardwalk running over the wetlands, which provides a good vantage point for observing local wildlife. Great blue heron, green heron, great egret, snowy egret, osprey, grackle, and red-winged blackbird are a few of the many bird species regularly seen on the lake. Bald eagles are occasionally seen on the Lake. The lake supports a healthy population of alligators and other reptiles and amphibians. Lake Howard is also known as a world class location with fresh water fishing, particularly for large mouth bass and bluegill. The Chain of Lakes Trail, a paved multi-use hiking and biking trail, begins here.</p><br>
<p>The Bowerman Barn is a historic barn located on Guy Covington Drive southwest of Trinity Center, California. The barn was built in 1878 by Jacob Bowerman, a local cattle rancher. Bowerman built the barn by hand with whipsawn pine wood and board and batten siding, and the barn is a relatively uncommon example of such a hand-crafted design. The barn served as part of Bowerman&#39;s ranch, which originally included a ranch house, milk house, and wagon shed, all of which burned down. Bowerman sold beef and dairy products to wholesalers and businesses in Minersville, and his business played a significant role in the development of the regional economy. Bowerman died in 1917, and the barn was subsequently used for sheep farming and storage until the USA Forest Service purchased the property in 1974.</p><br>
<p>The barn was added to the National Register of Historic Places on March 20, 1981.</p><br>
<p>The Greenwood Stage Station was a historic stagecoach stop located in what is now rural Morrill County, Nebraska. It was the second stage station on the Sidney-Black Hills Trail, when coming north from the Union Pacific railroad at Fort Sidney, Nebraska, on the way to gold mining fields in Montana. It played a significant role along the trail, serving travellers as a hotel, restaurant, and stable, as well as furnishing fresh horses for stagecoaches.</p><br>
<p>The archaeological site at the stations former location, denoted 25MO32, is a historic archaeological site that was listed on the National Register of Historic Places in 2012. Its significance arises from its status as one of the trails few remaining stage stations with extant artifactual and structural remains.</p><br>
<p>Its location is not revealed by the National Register, which lists it as "Address Restricted". It was listed as an archeological site with potential for future information.</p><br>
<p>The Menter Farmstead, near Big Springs, Nebraska, United States, was listed on the National Register of Historic Places in 2011. It is a farmstead built 1919–1928 during a regional agricultural boom sparked by winter wheat demand in World War I, and reflecting increased mechanization with its grain elevator and concrete block construction.</p><br>
<p>The most significant historic structure is the approximately 100 x barn, built c.1919. It has a complex roof with eaves and original wood shingles, built upon lower concrete block walls and a concrete foundation. It has been termed a variation of the "Midwest Three Portal Barn" type.</p><br>
<p>The listing on the National Register in 2011 included several contributing and non-contributing buildings.</p><br>
<p>The Sedgwick County Courthouse, located at 315 Cedar St. in Julesburg, Colorado, was built during 1938-39 by the Works Progress Administration . It was listed on the National Register of Historic Places in 2007; the listing included two contributing buildings.</p><br>
<p>It was deemed significant in social history for representing federal relief programs; its construction provided "much needed assistance by giving jobs to the unemployed of the county during the Great Depression."</p><br>
<p>It also was deemed significant architecturally, as "an excellent example of the Art Deco style as applied to a government building whose construction was constrained by the economic conditions of the Depression." It was designed by Jamieson and Stiffler, architects of Denver.</p><br>
<p>Selborne Hill is one of the highest points in the county of Hampshire, England. It is one of the East Hampshire Hangers, a line of prominent hills on the eastern scarp slope of the Hampshire Downs, and reaches 211 m above sea level. Its prominence of 53 metres qualifies it as one of the county&#39;s Tumps.</p><br>
<p>Selborne Hill lies above the village of Selborne on the edge of the Hampshire Downs, its crown playing host to Selborne Common, an area of woodland and relict wood-pasture. Its summit and steep escarpment are covered by woods, with Selborne Hanger to the northeast dropping abruptly to the fields above Selborne. The Zig-Zag Path runs down the spur towards the east. This is the area where the world famous naturalist and pioneer of birdwatching, Rev. Gilbert White, wrote his celebrated Natural History of Selborne.</p><br>
<p>Sawtooth Mountain is a shield volcano, and part of the polygenetic Indian Heaven Volcanic Field in Washington, United States. It is located midway between Mount St. Helens and Mount Adams, and dates from the Pleistocene and Holocene. Sawtooth Mountain is the third highest point at 5,354 ft. The mountain forms a series of welded volcanic rock spires, an eroded remnant of an ancient shield volcano. Sawtooth Mountain is the third highest point in the Indian Heaven Wilderness Area. While Sawtooth Mountain is not the highest, its craggy appearance makes it one of the most namesake peaks in the Indian Heaven Volcanic Field.</p><br>
<h2>Geographical setting</h2><br>
<p>Sawtooth Mountain is the third highest peak the Indian Heaven Wilderness in Washington and the Cascade Range. On clear days hikers can see views of four nearby volcanoes: Mount Adams, Mount Hood, Mount St. Helens, and Mount Rainier from the Sawtooth Mountain Trail, which skirts the subalpine upper west side of Sawtooth Mountain.</p><br>
<p>The shield volcano is noted as a series of eroded, volcanic spires. While the mountain is free of snow and ice, snow tends to linger on the summit well into July.</p><br>
<h2>Geology</h2><br>
<p>Sawtooth Mountain is one of the many shield volcanoes topped by cinder cones and spatter cones that make up the Indian Heaven Volcanic Field. About 60 eruptive centers lie on the 30 km long, N10°E-trending, Indian Heaven fissure zone. The 600 km&sup2; field has a volume of about 100 km3 and forms the western part of a 2,000 km&sup2; Quaternary basalt field in the southern Washington Cascades, including the King Mountain fissure zone along which Mount Adams was built.</p><br>
<h2>Climbing and recreation</h2><br>
<p>Popular fishing and hiking destinations in the volcanic field around Sawtooth Mountain include the Indian Heaven Wilderness, which is rather popular for the high mountain meadows among its scattered volcanic peaks. The Pacific Crest National Scenic Trail passes north/south through the volcanic field and the Indian Heaven Wilderness, which is known for its many lakes and spectacular views of four nearby volcanoes: Mount Adams, Mount Hood, Mount St. Helens, and Mount Rainier. It also hugs the densely forested east side of Sawtooth Mountain, and in conjunction with the Sawtooth Mountain Trail, can be hiked in a loop beginning at the Sawtooth Trailhead. Wood Lake is to the west of the peak, and a spur trail (Wood Lake Trail) leaves the Pacific Crest Trail for the lake. Major trails at Sawtooth Mountain are the Sawtooth Trail, which climbs up and skirts the upper west side of Sawtooth Mountain; and Wood Lake Trail, which descends west from the Pacific Crest Trail to the deep blue Wood Lake. The Pacific Crest Trail skirts the densely forested lower west side of the peak.</p><br>
<p>The Sawtooth Berry Fields is located just north of Sawtooth Mountain, around Surprise Lakes and the Sawtooth Trailhead for the Pacific Crest Trail.</p><br>
<p>The Fred and Minnie Meyer Sudman House, located at 490 Vincent Ave. in Chappell, Nebraska, is a historic house  that is a notable local landmark. It is a 42 x wood-frame house on a concrete masonry foundation. It is described as a "two-story, symmetrical, central hall, double-pile house," but having a plan that "incorporates spatial design usually reserved for high-style dwellings." It is known to have been built by contractor Henry Dickmeyer, but details of its designer are lost.</p><br>
<p>It was listed on the National Register of Historic Places in 1990. At the time of its NRHP listing, it was noted that a widow&#39;s walk that was "originally located on the truncation of the hip roof" had been removed, and accompanying 1988 photos showed no such walk; the photo in 2011 suggests that it has since been restored.</p><br>
<p>It has also been designated as NEHBS # DU02-2.</p><br>
<p>The house has now been restored to an early 20th-century appearance and is operated as the Sudman-Neumann Heritage House Museum.</p><br>
<p>The Prospect Peak Fire Lookout is a fire lookout station located on Prospect Peak in Lassen Volcanic National Park, near the city of Mineral, California. The lookout, which was built circa 1912, is one of the oldest extant USA Forest Service fire lookouts in the United States. The wood frame building is square with a pyramidal roof; its walls are mostly composed of tall windows, with shiplap siding below the windows and on the roof. This design was a standard design used by USA Forest Service fire lookouts at the time, and several of the other contemporary lookouts in the national park also used this style of construction. The lookout is likely now the only surviving station with this design. Though the station was ultimately abandoned and has lost its original windows and roof shingles, it is otherwise intact.</p><br>
<p>The lookout was added to the National Register of Historic Places on March 30, 1978.</p><br>
<p>The Union Pacific Railroad Julesburg Depot, at 210 W. First St. in Julesburg, Colorado, and also known as the Depot Museum, was built in 1930. It is listed on the National Register of Historic Places.</p><br>
<p>It is a brick, one-story building built as a standard Union Pacific Railroad "combination-type" depot, i.e. handling passengers as well as freight and express shipments.</p><br>
<p>The depot was hit by a tornado on June 6, 1947 that badly damaged the building; it was repaired. In 1974 it was moved a short distance and turned into a museum.</p><br>
<p>It was listed on the National Register in 2004. It was deemed significant for its role in transportation and the economic growth of Julesburg, and architecturally for its design, materials, and workmanship which are preserved despite the building having been moved a short distance.</p><br>
<p>Brimmond Hill is a hill in Aberdeen, Scotland that rises to a height of 266 metres. The summit is the highest point within the Aberdeen City council area.</p><br>
<p>The hill itself is situated in the area between Kingswells, Westhill, Blackburn and Dyce. There is a transmitter on the top of the hill, and there are also paths and a road to the top of the hill. The hill can be reached directly from paths that connect to Kingswells, and at the summit a view across the city of Aberdeen is available.</p><br>
<h2>Transmitter site</h2><br>
<p>The top of the hill has a collection of transmitter sites for microwave transmission, by line-of-sight communication. The communication sites from here have direct links between North Sea Oil platforms and their headquarters in Aberdeen.</p><br>
<p>Little Nescopeck Creek is a tributary of Nescopeck Creek in Luzerne County, Pennsylvania, in the United States. It is approximately 8.5 mi long and flows through Butler Township, Sugarloaf Township, and Conyngham. The watershed of the creek has an area of 14.0 square miles. The creek is acidic and receives mine water from the Jeddo Tunnel. The main rock formation in the watershed is the Mauch Chunk Formation. However, the Pottsville Formation also appears in some areas. Soil series in the drainage basin include the Arnot Series, the Basher Series, and various other soil types.</p><br>
<p>There is one source of acid mine drainage in the watershed of Little Nescopeck Creek: the Jeddo Tunnel. Major roads in the creek&#39;s watershed include Interstate 80, Pennsylvania Route 93, and Pennsylvania Route 309. Additionally, wetlands occur in the drainage basin. The watershed of the creek was inhabited by 8000 B.C.E. However, European settlers did not arrive until the 18th century. The Sugarloaf Massacre occurred near the creek in 1780. Recreational opportunities in the watershed include swimming and boating, and there are golf courses, public parks, and rail-trails in within the watershed.</p><br>
<p>The watershed of Little Nescopeck Creek is designated as a Coldwater Fishery and a Migratory Fishery. Several fish species inhabit the creek near its headwaters, but there is no aquatic life downstream of the Jeddo Tunnel. Fourteen amphibian species and eight reptile species also inhabit the watershed; some of them breed there as well. Dozens of species of insects and macroinvertebrates live in the creek&#39;s drainage basin. Common mammals include white-tailed deer, cottontail rabbits, and others. Plants inhabiting the watershed include conifer and hardwood trees, herbs, legumes, and grasses.</p><br>
<h2>Course</h2><br>
<p>Little Nescopeck Creek begins in a valley near Prospect Rock in Butler Township. It flows west-southwest for a few tenths of a mile before turning west-northwest as its valley broadens. The creek crosses Pennsylvania Route 309 before turning west-southwest after more than a mile. It then turns west-southwest for several miles, crossing Interstate 81 and entering Sugarloaf Township, where it flows along the base of Butler Mountain. In Sugarloaf Township, the creek turns northwest for several tenths of a mile, passing through Conyngham before turning north. Several tenths of a mile further downstream, it reaches its confluence with Nescopeck Creek.</p><br>
<h2>Hydrology</h2><br>
<p>Before the Jeddo Tunnel was constructed, Little Nescopeck Creek was around ten feet wide. This is also ten times wider than the creek was in the early 18th century. However, other factors besides the Jeddo Tunnel, such as discharges from sewage treatment plants and an increase in storm water runoff have also contributed to the widening of the creek. Plans to fix the pollution of Little Nescopeck Creek via the Jeddo Tunnel include reducing the tunnels discharge and the construction of wetlands. Little Nescopeck Creeks discharge upstream of the Jeddo Tunnel is 2.18 cubic feet per second. Downstream of the tunnel, the discharge is 60.02 cubic feet per second. The creek&#39;s specific conductance upstream of the Jeddo Tunnel is 178.3 micromhos per centimeter. Downstream of the tunnel, the specific conductance is 446.13 micromhos per centimeter.</p><br>
<p>The average level of precipitation in the Little Nescopeck Creek watershed between 1932 and 1998 was 49 inches per year.</p><br>
<h3>Water quality</h3><br>
<p>Between 1996 and 1998, the average pH of Little Nescopeck Creek was 4.6. During the same period, the waters of the creek contained an average of 130.87 milligrams per liter of sulfate, 4.03 milligrams per liter of aluminum, 2.01 milligrams per liter of iron, 1.83 milligrams per liter of manganese, and 0.31 milligrams per liter of zinc.</p><br>
<p>Upstream of the Jeddo Tunnel, the manganese concentration of the water of Little Nescopeck Creek averages around 108 micrograms per liter. Downstream of the tunnel, the average manganese concentration is 3320 micrograms per liter. Upstream of the tunnel, the average aluminum concentration is under 200 micrograms per liter. Downstream of the tunnel, the average aluminum concentration is 7470 micrograms per liter. Upstream of the tunnel, the average iron concentration is 380 micrograms per liter. Downstream of the tunnel, the average iron concentration is 1947 micrograms per liter. Upstream of the tunnel, the average nickel concentration is below 50 micrograms per liter. The average nickel concentration for the whole watershed is almost three times higher, at 144 micrograms per liter. The average zinc concentration is under 10 micrograms per liter above the Jeddo Tunnel but 519 micrograms per liter downstream of the tunnel. The calcium average concentration above the tunnel is 16.2 milligrams per liter. The average calcium concentration below the tunnel is 32.5 milligrams per liter.</p><br>
<p>There are between 10 and 36 micrograms per liter of copper in nine different sites in and near Little Nescopeck Creek. There are between 1 and 3.3 micrograms per liter of lead at these sites on the creek. There are between 10 and 621 micrograms per liter of zinc at these sites. The average concentration of sulfates upstream of the Jeddo Tunnel is below 10 milligrams per liter, but it is 257 milligrams per liter downstream of the tunnel. The average concentration of calcium carbonate upstream of the tunnel is 33 milligrams per liter, and downstream of it, it is 272 milligrams per liter.</p><br>
<p>The are also a number of non-metallic pollutants in the Little Nescopeck Creek watershed. Ammonia is one such pollutant, although the Jeddo Tunnel contributes little to the creek. There is also phosphorus and nitrite in the creek, but the tunnel does not contribute a measurable amount of such compounds.</p><br>
<p>In three different sites on Little Nescopeck Creek downstream of the Jeddo Tunnel, the daily load of aluminum passing through ranges from 2871 to 3175 lb. In the same sites, the daily load of iron ranges between 859 and. The daily load of manganese at the sites ranges from 1350 to 1432 lb. At one site upstream of the Jeddo Tunnel, these values are much lower. The daily load of aluminum is 2.8 lb, the daily load of iron is 11.3 lb, and the daily load of manganese is 2.6 lb.</p><br>
<h2>Geography and geology</h2><br>
<p>The elevation near the mouth of Little Nescopeck Creek is 860 ft above sea level. The elevation of the creek&#39;s source is between 1,420 and above sea level. The creek is in the ridge and valley physiographic province.</p><br>
<p>Little Nescopeck Creek is mostly situated on top of the Mauch Chunk Formation, a Mississippian period rock that consists of shale, conglomerate, and coarse gray sandstone. Areas containing the Mauch Chunk Formation in the watershed include the bottom of the Little Nescopeck Creek valley and Nescopeck Mountain. The Pottsville Formation is another formation in the creek&#39;s watershed. It consists of coarse sandstone, gray quartz conglomerate, and shale with some coal. The Pottsville Formation is found in small amounts on Nescopeck Mountain. There is no coal in the watershed of Little Nescopeck Creek. The watershed has never been mined.</p><br>
<p>There are several main types of soil in the watershed of Little Nescopeck Creek. Two of them are the Arnot Series and the Alluvial land. The Arnot Series soil is shallow and drained well. It ranges between close to flat and steep. The Alluvial land ranges between close to flat and moderately sloping. It contains gravel and stones and is found along flood plains within the watershed. A large number of other types of soils are found in very small amounts in the creek&#39;s watershed. One type of soil that is also found in the Little Nescopeck Creek watershed is the Basher Series. Along the creek near Sybertsville, this type of soil is reddish-brown and sticky to a depth of six there inches (15 centimeters). From 6 to 18 inches (15 to 45 centimeters), the soil is reddish-brown with some areas of yellowish-red. From 18 to 24 inches (45 to 60 centimeters), the soil is reddish-brown with pinkish-gray areas and is a sandy loam. From 24 to 37 inches (60 to 93 centimeters), the soil is reddish-brown with pinkish-gray areas and is a sandy loam. From 37 to 47 inches (93 to 118 centimeters), the soil is reddish-brown with light gray and yellowish-red areas, and is a coarse sandy loam. From 47 to 53 inches (118 to 133 centimeters), the soil is a reddish-gray sandy loam with some yellowish-red areas. From 53 to 62 inches (133 to 156 centimeters), the soil is reddish-gray and contains sand and gravel.</p><br>
<p>The creek&#39;s river valley is steep and narrow. Nescopeck Mountain is in the northern part of the watershed and Buck Mountain is in the southern part. The elevation in the watershed ranges from between 850 and 1800 feet. There is very little limestone near the creek, thus making it very acidic.</p><br>
<p>There are several floodplains in the watershed of Little Nescopeck Creek. The largest of them is near where the creek turns northward, but there is also one not far from the its headwaters.</p><br>
<h2>Watershed</h2><br>
<p>The watershed of Little Nescopeck Creek has an area of 14.0 square miles. The watershed extends over Sugarloaf Township, Butler Township, Conyngham, and an extremely small part of Hazle Township. The communities of Drums and Kis-Lyn are also in the watershed. The Little Nescopeck Creek watershed is bordered by the Black Creek watershed to the south and the main stem of Nescopeck Creek to the north.</p><br>
<p>The Little Nescopeck Creek watershed is affected by pollution from the Jeddo Tunnel. However this is the only source of acid mine drainage in the watershed. The pollution of the Jeddo Tunnel affects Nescopeck Creek, the Susquehanna River, and the Chesapeake Bay. The creek&#39;s watershed consists mostly of farmland and suburbs. However, there are also some woodlands and riparian buffers. The major highways in the Little Nescopeck Creek watershed are Interstate 80, Pennsylvania Route 93, and Pennsylvania Route 309.</p><br>
<p>There are a number of different types of wetlands in the Little Nescopeck Creek watershed. One type of wetland is the various palustrine, which is scattered in small areas along the creek. The palustrine forested wetland is the type of wetland that makes up the largest patch of wetland in the creeks watershed. This patchs dimensions are 1 mi by 0.1 mi. In the northeastern part of the watershed there are palustrine shrub-scrub, deciduous, broad-leaved evergreen wetlands. In the northwestern portion of the watershed there are palustrine unconsolidated bottom and palustrine forested broad-leaved deciduous wetlands.</p><br>
<h2>History</h2><br>
<p>The area in the vicinity of Little Nescopeck Creek was inhabited by Native Americans as early as 8000 B.C. Some of the earliest people to settle in the Little Nescopeck Creek watershed were the Lenni Lenape. European occupation of the creek&#39;s watershed began at the middle of the 1700s. The construction of the Susquehanna and Lehigh Turnpike also helped to increase the population of the Little Nescopeck Creek watershed.</p><br>
<p>The Sugarloaf Massacre occurred near Little Nescopeck Creek on September 11, 1780. In 1809, Redmond Conyngham built a sawmill on M. Beishline&#39;s land on Little Nescopeck Creek in southwestern Butler Township. In 1810, a carding mill was built on the creek in what was then known as the community of Ashville. Redmond Conyngham also built a gristmill across the creek from the sawmill in 1814. Phillip Drum built a woolen mill near the carding mill in 1835. The creek flooded during Hurricane Agnes in 1972.</p><br>
<p>There are a number of historical sites in the Little Nescopeck Creek watershed. Most of them are devoted to the anthracite industry. Little Nescopeck Creek&#39;s name comes from a Lenni Lenape word meaning "deep black river".</p><br>
<p>In 1995, a $50,000 grant was given to the Wildlands Conservacy to improve the water quality of Little Nescopeck Creek. Since the beginning of the 21st century, traffic in the Little Nescopeck Creek watershed has multiplied fourfold. The Environmental Protection Agency has established five sites along Little Nescopeck Creek. They are called LNESC5, LNESC6, LNESC7, and LNESC9. The last of these is upstream of the Jeddo Tunnel, but the other sites are downstream of the tunnel.</p><br>
<h2>Biology</h2><br>
<p>The drainage basin of Little Nescopeck Creek is designated as a Coldwater Fishery and a Migratory Fishery. However, downstream of the Jeddo Tunnel there is no aquatic life. Although there are plans to restore the fish population on the creek, such plans are impossible to carry out in the near future, due to the expense that would be required for such a restoration. Near the creek&#39;s headwaters there are sunfish, brook trout and brown trout and bass. The brown trout and brook trout are native. In 1998, a total of 56 fish over eight different taxa were discovered upstream of the Jeddo Tunnel. The most common species were creek chub and white sucker. One brook trout was discovered in the creek. Upstream of the Jeddo Tunnel, there are also turtle and salamander populations. There are a total of 14 species of amphibians in the watershed. Of these, ten species breed in the watershed. There are also a total of eight species of reptiles in the watershed. They consist of two turtles and six snakes. Only the two turtles breed in the watershed. Additionally, there are more than 50 species of birds in the watershed.</p><br>
<p>The most common large game animal in the Little Nescopeck Creek watershed is the white-tailed deer. Cottontail rabbits are also common in the watershed, especially in the areas devoted to farming. Beavers, raccoons, and muskrats are the most common fur-bearing animals in the watershed.</p><br>
<p>The macroinvertebrates in the area of Little Nescopeck Creek include five species of flies, five species of caddisflies, four species of mayflies, three species of stone flies, two species of alder flies, two species of beetles, one species of gastropod, and one species of sow bug. There are 30 species of butterflies on the watershed of Little Nescopeck Creek. Of these, seven breed in the creeks watershed. The creeks watershed is also home to seven species of dragonflies and damselflies. Of these, three species breed in the creek&#39;s watershed.</p><br>
<p>Common plants in the Little Nescopeck Creek watershed include conifer and hardwood trees, herbs, legumes, and grasses. The plants in the Little Nescopeck Creek watershed are fairly typical for the Ridge-and-Valley province. Resident deciduous trees in the watershed include five species of oak, one species of cherry, five species of maple, one species of walnut, two species of hickory, and four species of birch, two species of dogwood, and one species each of basswood, poplar, ash, and beech. All but four of these trees are found in the creeks riparian zone. Coniferous trees in the watershed include three species of pine, two species of spruce, and one species of hemlock. Four of these species are found in the creeks riparian zone. There are also 16 species of legumes, grasses, and weeds, seven species of bushes, and six species of perennials. All of the bushes and perennials, and seven of the grasses are found in Little Nescopeck Creeks riparian zone. There are also a number of aquatic plants in Little Nescopeck Creek. These include bulrush, pondweed, duckweed, waterweed, and some types of algae, all of which are typical for a stream in the eastern United States. The forest around the creeks headwaters are composed mostly of oak and hickory.</p><br>
<p>Little Nescopeck Creeks riparian zone has survived to date due to conservation efforts of the local community. The narrowest area of the riparian zone is zero feet in a pasture one mile upstream of the Jeddo Tunnel. The widest area of the riparian zone is 500 ft on the Keystone Jobs Corps Center property. At Little Nescopeck Creeks confluence with Nescopeck Creek, the riparian zone is 100 ft wide or more.</p><br>
<p>There are a total of five species of special concern in the Little Nescopeck Creek watershed. These include the mountain starwort, which is critically endangered in Pennsylvania.</p><br>
<h2>Recreation</h2><br>
<p>There are few opportunities for activities in Little Nescopeck Creek itself, such as swimming and boating. However, there are some golf courses, public parks, and rail-trails within the creeks watershed. The four golf courses are the Sugarloaf Golf Course, the Sand Springs Golf Course, the Edgewood in the Pines Golf Course, and the private Valley Country Club. There are three recreational sites in the creeks watershed. One is the Butler Recreation Complex in the eastern part of the watershed. The other two are the Whispering Willow Park and the Historic Brainard Church in the western part of the watershed.</p><br>
<p>In 1998, there were plans to convert abandoned railroad beds in the Little Nescopeck Creek watershed to rail-trails. There are already a number of trails in the watershed. Some of these date back to Native American times. There are also a number of outlooks in the creek&#39;s watershed. There is some kayak traffic on the creek during the spring. There is a 24-acre area of fields and woodlands known as the Bishop Tract; a portion of this tract is along Little Nescopeck Creek.</p><br>
<p>The Yorba-Slaughter Adobe is a historic adobe house located at 17127 Pomona Rincon Road near Chino, California. Built in the early 1850s, the adobe is typical of the building style prevalent during and around California&#39;s period of Mexican governance. Raimundo Yorba built the adobe on land thought to be part of Rancho El Rincon, a land grant owned by his father, Bernardo Yorba; however, a later survey determined the adobe was not part of the rancho. The younger Yorba lived in the adobe until 1868, when Forty-Niner and Mexican-American War veteran Fenton M. Slaughter bought the house. Slaughter, who later served in the California State Assembly, lived in the house until his 1897 death.</p><br>
<p>Slaughter&#39;s daughter, Julia Slaughter Fuqua, began rehabilitating the adobe in 1928. The adobe was designated a California Historical Landmark on June 20, 1935. It was added to the National Register of Historic Places on July 7, 1975.</p><br>
<p>The adobe now functions as a branch museum of the San Bernardino County Museum and includes an 1890s period general store.</p><br>
<p>Fort Collins Armory in Fort Collins, Colorado is a historic armory building designed by Denver architect John J. Huddart or a Mr. Garbutt. It may date to 1907.</p><br>
<h2>History</h2><br>
<p>An armory in Fort Collins was constructed in 1907 based on a design by S.H. Clammer and F.A. Carleton. It included a basement shooting gallery, a large drill hall, officers quarters, enlisted mens quarters, and offices. used as a meeting, convention, and entertainment facility. It was replaced in 1922 with a new building. After its construction in 1907, Fort Collins’ historic Armory building often functioned as a space for public gathering and entertainment. The building served as the community’s first permanent National Guard Armory, housing about 60 National Guardsmen. Its drill hall doubled as a public hall for Northern Colorado&#39;s social and civic events. When a new armory was built on College Avenue in 1922, the building was vacated by the National Guard. Since then, the Armory building on Mountain Avenue has served the community in various ways, including as a roller skating</p><br>
<p>rink, a laundry, a meeting hall, and office and retail space. In 2014, the Armory held its first event as a music venue; Bohemian Nights Presents Concerts at the Armory.</p><br>
<p>The Carnegie Library, historically known as the Upland Public Library, is a Carnegie library located at 123 East D Street in Upland, California. Built in 1913, the library was the first public building in Upland. Architect Homer W. Glidden designed the library in the Classical Revival style. The library&#39;s design features a projecting central entrance with a plain frieze supported by two columns and brick pilasters, a stucco parapet extending around most of the building, and a cornice set above dentils. The building served as a library until 1969, when the library moved to a new building. The City of Upland still owns the building, which it rents to the public for community events and is used by the Upland Public Library to house its Literacy Program.</p><br>
<p>The library was added to the National Register of Historic Places on December 10, 1990.</p><br>
<p>Bellevue, also known as Wavertree Hall Farm, is a historic home and farm complex located near Batesville, Albemarle County, Virginia. The main house was built in 1859, and is a two-story, hip-roofed brick building with a two-story pedimented portico. It features wide bracketed eaves in the Italianate style and Greek Revival trim and woodwork. There are two 1 1/2 story brick wings on either side of the main block added about 1913, and a two-story brick south wing added in the 1920s. Also on the property are an antebellum log slave house, several tenant houses, a pump house, chicken house, and stable and barns. There is also an unusual underground room built into the north side of one of the garden terraces.</p><br>
<p>It was added to the National Register of Historic Places in 1991.</p><br>
<p>Blenheim is a historic home and farm complex located at Blenheim, Albemarle County, Virginia. The main house was built by politician and diplomat Andrew Stevenson in 1846, and is a 1 1/2-story, six bay, gable-roofed frame building with Gothic Revival and Greek Revival style details. It has an ell at the rear of the west end. The front facade features a pair of one-story tetrastyle porches with pairs of Doric order piers. A notable outbuilding is the square "Athenaeum", a one-story, one-room, frame Greek Revival building with a pyramidal hipped roof and portico supported on Doric piers. Also on the property are a frame kitchen/laundry, a "chapel" or schoolhouse, and two smoke houses. Also on the property are two dwellings, one of which is supposed to have been built to accommodate Justice Roger B. Taney on his visits to Blenheim. The main house and many of the outbuildings were built during the ownership of Representative Andrew Stevenson , who purchased the property in 1846.</p><br>
<p>It was added to the National Register of Historic Places in 1976.</p><br>
<p>The Arizona Rancho, also known as the Higgins House, Brunswick Hotel and Arizona Hotel, is a former hotel in Holbrook, Arizona. It was originally built between 1881 and 1883 as a residence, the expanded as a boarding house, a hotel, and finally as a motel. The original structure is thought to be the oldest extant structure in Holbrook.</p><br>
<h2>History</h2><br>
<p>The original house was built by Pedro Montaño, probably as a single-story house, using plastered adobe. With its dormers and steeply-pitched roof, it represents a hybrid of Hispanic and Anglo building styles. The house was expanded about 1885 with a two-story wing of adobe bricks, the Higgins addition, after an 1884 sale of the property to James and Maggie Higgins, who established a boarding house. After several changes of ownership, the Higgins House became the Brunswick Hotel after 1889, operated by John and Anna Connor. The upstairs portion of the addition was used as a dance hall and as a Masonic lodge. After several more changes of ownership the property was bought by S. Earle Taylor, an oil investor, to house workers. The property has remained in the Taylor family since then. Lloyd Taylor, a geologist, bought the hotel from his uncle.</p><br>
<p>During the 1930s the west wing of the Brunswick Hotel was Holbrooks hospital. A kitchen addition, necessitated by this change was designed in the mid-1930s by Lorimore Skidmore. Skidmore went on to design the later additions after the hotel became the Arizona Hotel. In the 1940s the compound was enclosed with an adobe wall, and adobe loggias were added, and the hotels name was hanged again to the Arizona Rancho. During World War II the hotel was leased by Fullerton Junior College to house pilot candidates training for the USA Navy at Park Field in Holbrook. The Taylor family added to the complex for their own living quarters at this time.</p><br>
<p>With the end of the war, business prospered. The hotel catered to tourists going to California on USA 66, which ran through Holbrook. However, the main road was farther north, and a new commercial district developed along 66 a few blocks to the north of the old town center, which had been oriented to the railroad line. The construction of Interstate 40 farther away caused further decline, leading to the hotel&#39;s closure after some time as a youth hostel.</p><br>
<h2>Description</h2><br>
<p>The Arizona Rancho compound is located on a corner lot to the south of the present Holbrook business district, between the railroad tracks and the Little Colorado River. The buildings are arranged on the north side of the site, facing an open, partially walled parking area. The wall is broken by openings with decorative wagon wheels set into the spaces, echoed by round window openings in the main building with inset wagon wheels. The complex is described as a "hodgepodge" of additions and styles. It retains a general Southwestern style with an emphasis on Pueblo Revival style, mainly expressed in the motel addition. The Montaño residence alone has a steeply-pitched roof, partly obscured by a later two-story adobe addition.The motel section is a long, low structure with projecting vigas over the fronting porch. Windows throughout the complex are framed in heavy wood timbers that are flush with the adobe plaster exterior wall finish. The motel wing includes a variety of wall materials, including stone, wood framing covered with stucco, and an adaptation of log-style construction with old wood posts laid up and chinked with stucco.</p><br>
<p>The Arizona Rancho was listed on the National Register of Historic Places on October 17, 1997. In 2007 plans were advanced to sell some surrounding properties and to restore the Rancho.</p><br>
<p>The San Bernardino County Court House, located at 351 N. Arrowhead Ave. in San Bernardino, is the county courthouse for San Bernardino County, California. The courthouse was built in 1927 and has served as the center of county government since then. San Bernardino architect Howard E. Jones designed the courthouse in the Classical Revival style; the courthouse is the only surviving Classical Revival building in San Bernardino. The building&#39;s design features classical columns spanning the second and third floors, a parapet along the roof line, regularly spaced windows, and extensive use of projecting blocks on the front facade. The courthouse is faced with unpainted stone and stucco, an uncommon design choice. A 1937 welfare building, a 1940 county library, and a 1940 heating plant are also located on the courthouse grounds, which are extensively landscaped and include a fountain, sundial, plaque, and the remains of the former county courthouse.</p><br>
<p>The courthouse was added to the National Register of Historic Places on January 12, 1998.</p><br>
<p>Oakham Hill is one of the highest points in the county of Hampshire, England, and in the South Downs, rising to 202 m above sea level.</p><br>
<p>Oakham Hill rises about 1 kilometre southeast of the village of Buriton in Hampshire and just a few hundred metres east of the county boundary with West Sussex. Just to the west are the summits of Head Down (205 m), War Down (244 m) and the highest point in the South Downs, Butser Hill (270 m), in the heart of the Queen Elizabeth Country Park. On the southern spur of Oakham Hill is Ditcham Park School, a private educational establishment.</p><br>
<p>Oakham Hill is also the site of the British Schools’ Cycling Association&#39;s National Hill Climb Time Trial, which in 2013 attracted one hundred and sixty competitors between the ages of 5 and 16, 34 of which were also pupils of Ditcham Park School.</p><br>
<p>The Pure Oil Station in Geneva, Illinois is a former gas station for the Pure Oil Company. The historic building was recognized by the National Park Service on its National Register of Historic Places on April 23, 2013.</p><br>
<h2>History</h2><br>
<p>The Pure Oil Station in Geneva, Illinois was built in 1937 on Illinois Route 38 (West State Street) at its intersection with Fifth Street. The Pure Oil Company popularized the idea of a filling station buildings. Prior to the 1920s, filling stations were regarded as unappealing fire hazards and were kept away from residential areas. Pure Oil developed a cheap, attractive design in the Tudor Revival style that fit the suburban aesthetic ideal. Pure Oil&#39;s design became their corporate trademark starting in 1927. Carl August Petersen, the Chief Engineer of Marketing Construction for Pure Oil, was responsible for the design which was replicated all over the country.</p><br>
<p>By 1945, there were six gas stations along the four blocks of downtown State Street. Only two remain—this station and an unnamed station of questionable integrity at 427 State Street. It is not a contributing property of the Central Geneva Historic District, but is within its physical boundaries.</p><br>
<h2>Architecture</h2><br>
<p>The main facade faces Illinois Route 38 to the north, and the east facade faces South Fifth Street. The exterior is brick, covered in white paint. The east section of the building serviced pedestrians and the west section serviced vehicles. The brickwork is decoratively skintled (bricks are irregularly projecting at varying degrees). Most of the building is covered with a steeply pitched gable roof. It is covered with blue terra cotta tile. A flat roof covers the south half of the service bays, though it is mostly hidden from view because of the pitched roof. Three brick chimneys flank the ends of the gables. Two of these chimneys have a large metal letter "P", painted white, a Pure Oil emblem.</p><br>
<p>The Gann Building is a historic building located at 218 S. Market St. in Benton, Arkansas. The building, which was built in 1893, is the only known extant building to have been built out of bauxite. Dr. Dewell Gann, Sr., had the building constructed as an office for his medical practice; the building was built by his patients in lieu of payment for medical services. After his office became successful, Gann helped establish the Saline County Medical Society. Gann&#39;s son, Dewell Gann, Jr., also worked in the office; Gann, Jr., was a successful physician as well and was named a Fellow of the Royal College of Surgeons of Edinburgh in 1925. The office was converted to a city library in 1946, and later became a local museum in 1967.</p><br>
<p>The Gann Building was added to the National Register of Historic Places on October 21, 1975.</p><br>
<p>Port Kembla is a man-made cargo port or artificial harbour, with an outer harbour protected by breakwaters and an inner harbour constructed by dredging, located in the Illawarra region of New South Wales, Australia.</p><br>
<p>Activities within the port are managed by the Port Kembla Port Corporation.</p><br>
<h2>Iron ore</h2><br>
<p>The first shipment of iron ore for use in Australian Iron and Steel&#39;s new blast furnace was received from Whyalla, South Australia in 1928. The ore shipment of 5,500 tonnes had been mined by the Broken Hill Proprietary Company at Iron Knob in the Middleback Ranges. In 1952 the first Yampi-class bulk carriers delivered iron ore to Port Kembla, carrying maximum loads of 11,000 tonnes.</p><br>
<h2>Location and features</h2><br>
<p>Located to the east of the Wollongong suburb of Port Kembla, the harbour of Port Kembla comprises a 8,439 ML body of water with a surface area of 1.4 km&sup2; at a dredged average depth of 6.1 m drawn from a catchment area of 6.3 km&sup2;.</p><br>
<p>The port of Port Kembla was established in the late 1890s to facilitate the export of coal from the mines of the Illawarra region. Diversification of the port facilities during the late-1980s and since, has seen the port to include general and break bulk cargoes, containers and motor vehicle imports, and bulk grain exports.</p><br>
<p>Regulation of the port rests with a number of federal, state, and local government agencies including the Australian Maritime Safety Authority, the Environment Protection Authority, and Wollongong City Council.</p><br>
<p>Faulkner House, also known as Seymour, Montesano, Garallen, and Old Ivy Inn, is a historic home located near Charlottesville, Albemarle County, Virginia. It was built in 1855-1856, and enlarged and remodeled in 1907 in the Colonial Revival style under the direction of architect Waddy B. Wood. The original section is the central two-story, brick structure topped by a hipped roof. In 1907, the house was enlarged with the addition of recessed, two-story, single-pile side wings and monumental front portico. Toward the end of the American Civil War, the house served as temporary headquarters of Union General Thomas Devin and was the home of Senator Thomas S. Martin from 1906 to 1919.</p><br>
<p>It was added to the National Register of Historic Places in 1984.</p><br>
<p>Birdwood is a historic home located on the grounds of the University of Virginia&#39;s Birdwood Golf Course near Charlottesville, Albemarle County, Virginia. It is a two-story, brick plantation house built between 1819 and 1830. The main house is a square, double-pile, central-passage plan house with four rooms on each floor and an entry portico supported by four monumental Doric order columns. A massive Colonial Revival addition was built in the early-20th century. Also on the property are a two-room stone plantation quarters, a stable and garage, and a distinctive lighthouse-shaped water tower, and traces of the late 19th or early-20th century ornamental gardens that include sculpture and an elaborate iron and fieldstone gate.</p><br>
<p>It was added to the National Register of Historic Places in 2003.</p><br>
<p>Mechum River Farm is an historic manor house and farm located near Charlottesville, Albemarle County, Virginia. The original house was built about 1820 presumably by a Burch family member, then updated and expanded about 1850 in the Gothic Revival style during the ownership of John C. Burch and Lucinda E. Gay Burch. It is a 1 1/2-story, three bay, brick hall and parlor plan dwelling set on a raised basement with a solid brick foundation and a side gable roof. It features a hipped-roof portico over the central single-leaf entry. It has a rear addition built about 1920 and an extension to that built in 1976. Also on the property are a contributing barn , shed , wood shed , Delco shed , smokehouse , chicken coop , privy , shed , and family cemetery.</p><br>
<p>It was added to the National Register of Historic Places in 2007.</p><br>
<p>Carrs Hill, also known as the University of Virginia Presidents House, is a historic home located near Charlottesville, Albemarle County, Virginia. Carr&#39;s Hill was built in 1906, and is a two-story, five bay brick dwelling in the Colonial Revival style. It features a prominent double-height pedimented portico in the Doric order a slate covered hipped roof, and two tall chimneys. It was designed by the prominent architectural firm of McKim, Mead & White. The house overlooks the university chapel and the "Academical Village." Also on the property are the contributing Guest Cottage , Buckingham Palace , the Leake Cottage , carriage house , the landscape , and two iron capitals  that were salvaged from the ruins of the Robert Mills Rotunda Annex after the 1895 fire.</p><br>
<p>It was added to the National Register of Historic Places in 2008.</p><br>
<p>Lewis Mountain, also known as Onteora, is a historic home located near Charlottesville, Albemarle County, Virginia. It was designed in 1909, and completed in 1912. The house is a three-part plan granite dwelling, consisting of a nearly square center section flanked by one-story, flat-roofed wings in the Colonial Revival style. It features a massive wooden cornice employing a simplified version of the Roman Doric order of Vignola, a deck-on-hip roof with pedimented dormers at its base, and a portico with four Doric order columns. It also has a one-story, tetrastyle Tuscan portico that serves as a</p><br>
<p>porte cochere. The steeply sloped property features a landscape designed by Warren H. Manning with a series of three terraces with tall dry-laid stone retaining walls.</p><br>
<p>It was added to the National Register of Historic Places in 2009.</p><br>
<p>Idebessos or Idebessus, also known as Edebessus or Edebessos  or , was an ancient city in Lycia. It was located at the foot of the Bey Mountains to the west of the Alakır river valley. Today its ruins are found a short distance to the west of the small village of Kozağacı in the Kumluca district of Antalya Province, Turkey. The site, 21 kilometres north-northwest of Kumluca, is overgrown with forest and hard to reach.</p><br>
<h2>Geography</h2><br>
<p>The city lies at an altitude of 1050 meters. Due to the nature of the terrain, the city was built in a north-south orientation and occupies approximately 360 by 160 meters. Larger public buildings and the necropolis were built on flatter areas in the west, while dwellings were mostly built on the sloping part of the terrain in the east. The eastern slope is widened by terrace walls at different elevations, which provided narrow corridors with primarily houses.</p><br>
<h2>History</h2><br>
<p>Except for a coin from the Classical period, which has been controversially attributed to the city, there is no evidence of the city&#39;s existence before the Hellenistic period. Idebessos was a member of the Lycian League from its foundation in 168 BC. Inscriptions mention that the city was a polis and a member of a sympoliteia with Akalissos and Kormos. The sympoliteia was led by Akalissos and represented by a single vote in the Lycian League during the Roman period.</p><br>
<p>A Lycian town named Edebessus (Ἐδεβησσός) is mentioned by the Lycian Capito in his Isaurica, an 8-volume history of Isauria. The Synecdemus lists Elebesus (Ἐλεβεσός), corrected to "Edebessus" (Ἐδεβησσός) in Wesselings 1735 edition, while Partheys 1866 edition suggests that it may correspond to the Λεβισσός or Λιβυσσός (Lebissus or Libyssus) mentioned in the Notitiae Episcopatuum. A report on archaeological investigations in 2005 also presumed an identity of Idebessus with the bishopric town of Lebissos or Lemissos. However, the list of titular sees (formerly residential) that are recognized by the Catholic Church includes both Idebessus (identified with modern Kozağacı) and Lebessus (identified with modern Kayaköy) and describes each as a suffragan of the metropolitan see of Myra, the capital of the Roman province of Lycia.</p><br>
<p>The city was still occupied in the Byzantine period, and it is not known when the city was deserted.</p><br>
<h2>Archaeological investigations</h2><br>
<p>T. A. B. Spratt identified the ruins of the city as the remains of Idebessos in 1842. In two days he surveyed the site and copied some inscriptions. Over time numerous other scholars visited the archaeological site for smaller investigations, but it was not until the 2000s that a detailed survey of all the remains was completed.</p><br>
<h2>Layout</h2><br>
<p>A main street entered the city to the west of the acropolis and then ran north. From the south to the north a Greek theater, a bath-gymnasium complex and a church are found along this road. The public center of the settlement is the area between the theater and the baths. A wide flat area between these buildings must have served as the agora.</p><br>
<p>The necropolis extends uninterrupted along the main street and is most dense in the city&#39;s center, which is quite unusual. Normally necropoleis were located along the main roads leading to the city and end outside the settlement. The baths, theater, northern church and the necropolis have been reasonably well preserved, but most of the houses are damaged to a level that it is not possible to determine their layout.</p><br>
<h3>Acropolis</h3><br>
<p>The acropolis covers an area of 120 by 150 meters in the southeast of the settlement, rising approximately 10 meters above the city&#39;s center. The northern and western sides of the acropolis were protected with walls reinforced with three towers. The eastern and southern sides of the acropolis were naturally protected by steep rock faces and had a terrace wall. A heroon from the Roman period and a Byzantine church from the 5th or 6th century AD were built on the acropolis.</p><br>
<p>In the Byzantine period the acropolis was transformed to a castrum with stronger fortifications. It encircled the church and was constructed with building material partially reused from the structures of the Roman period. It must have been built in the 7th or 8th century AD, when the region was subject to increasing Arab raids as a consequence of the Arab–Byzantine wars.</p><br>
<h3>Other structures</h3><br>
<p>The Greek theater dates to the Hellenistic period. It was built into the northwestern slope of the acropolis hill and has been estimated to seat a maximum of 364 people. The bath-gymnasium complex was most likely built no later than the 2nd century AD and consists of seven separate units and a palaestra. The baths were supplied with water from a stream to the north of the city by a small canal. The northern church is the largest church of the settlement, measuring about 15.30 by 28.15 meters and likely built in 5th or 6th century AD. A small triconch church is found south in the city, but is completely ruined. It was possibly built later than the two other churches. The necropolis counts 51 sarcophagi and four exedra-type tombs.</p><br>
<p>Cobham Park, or Cobham Park Estate, is a historic estate located near Cobham, in Albemarle County and Louisa County, Virginia. The mansion was built in 1856, and is a rectangular 2 1/2-story, five bay, double pile structure covered by a hipped roof with three hipped roof dormers on each of the main slopes, and one dormer on each end. The house is an unusual example of ante-bellum period Georgian style architecture. It features front and rear, simple Doric order porches supported on square Ionic order columns. Also on the property are two smokehouses, one brick and one frame, a frame dependency, and a simple two-story</p><br>
<p>frame dwelling. It was the summer home of William Cabell Rives, Jr., (1825-1890), second son of the noted United States senator and minister to France William Cabell Rives.</p><br>
<p>It was added to the National Register of Historic Places in 1974.</p><br>
<p>Jones Pass, elevation 12,454 ft, is a mountain pass that crosses the Continental Divide in the Front Range of the Rocky Mountains of Colorado in the United States.</p><br>
<p>The Gumlick Tunnel is a water tunnel under Jones Pass for water diversion from the upper Williams Fork east under the continental divide into the valley of Clear Creek (Colorado). The water is not discharged into Clear Creek, but is sent north through the Vasquez Tunnel which passes back under the continental divide. The water is eventually delivered to the City of Denver via the Moffat Tunnel. The 2.9 mile (4.7Km) Gumlick Tunnel was completed in 1940 and significantly improved in 1957-58. The tunnel is horseshoe-shaped, 7 feet (2.1m) high, and can carry water at 550 cubic feet per second (15.6m/s).</p><br>
<p>Hot Lake is a hypersaline, meromictic lake located in extreme northern Okanogan County, Washington near Oroville, Washington. Occupying a small, glacially-carved basin surrounded by mafic magnesian rocks, dolomites, and shales containing deposits of pyrite and pyrrholite minerals, Hot Lake is unusual among hypersaline lakes in that it is dominated by magnesium and sulfate as its major ions. Because of its mineralogy, Hot Lake was mined for epsomite, initially by the Stewart-Calvert Company during World War I, when the importation of epsomite from Germany was suspended. Major flora growing within the lake include Ruppia maritima and Chara, and the dominant fauna are the brine shrimp Artemia salina and Branchinecta campestris. A benthic phototrophic microbial mat dominated by cyanobacteria is also found within the lake.</p><br>
<p>Farmers Bank of Carson Valley  is a historic bank building located at 1596 Esmeralda Avenue in Minden, Nevada. The building was built in 1909 to house the Farmer&#39;s Bank of Carson Valley, which was chartered in the same year. H. F. Dangberg, the founder of Minden, commissioned the building, which was only the second building built in the town. In 1918, the bank outgrew its original building and moved to a larger building across the street. After the bank left the building, it was occupied by the Minden Post Office until 1974. The building has housed a variety of businesses since and is currently occupied by the Bank Parlor and Pub.</p><br>
<p>The building was added to the National Register of Historic Places on April 6, 2000.</p><br>
<p>Farmers Bank of Carson Valley  is a historic bank building located at 1597 Esmeralda Avenue in Minden, Nevada. The bank was built from 1916 to 1918 to replace the original 1909 bank building, which the Farmers Bank had outgrown. Prominent Nevada architect Frederic Joseph DeLongchamps designed the building in the Classical Revival style; the bank is one of many Neoclassical structures designed by DeLongchamps in Minden. The banks design features a cornice with terra cotta tiles and bands, a flat roof with a low parapet, and an entrance portico with Ionic columns. The bank was built for Farmers Bank organizer H. F. Dangberg, who was also the founder of Minden. The building served as a bank until 1968 and currently houses offices.</p><br>
<p>The building was added to the National Register of Historic Places on August 6, 1986.</p><br>
<p>Manitou Bathhouse or Manitou Spa is a historic building located along Fountain Creek in Manitou Springs, Colorado. Once used as a mineral water bathhouse or spa, the building is now used for stores and other businesses on the first floor. The second and third floors hold residential units. It is on the National Register of Historic Places. Located in the building is Adam&#39;s Mountain Cafe.</p><br>
<p>The Manitou Spa building is located near several natural mineral springs and within the building is the Soda Spring. The spa was the "town&#39;s social center" in the early 1900s.</p><br>
<p>The building, constructed in 1920</p><br>
<p>The original bathhouse was built in 1882 to 1883 and was torn down in 1923, or in 1921. Visitors to the bathhouse could bathe in a cool plunge pool, relax in hot mineral water baths, visit the physician or relax in one of the reading rooms.</p><br>
<p>The Carson Valley Improvement Club Hall is a historic building located at 1606 Esmeralda Avenue in Minden, Nevada. The building was constructed in 1912 as a meeting hall for the Carson Valley Improvement Club. The two-story building features a variety of brickwork patterns but has an otherwise plain design. The Carson Valley Improvement Club used the building to host both community social events and town meetings. The building has served as the informal seat of government in Minden since its construction; after the Carson Valley Improvement Club moved out in 1920, the Minden Commercial Club and later the Minden Town Board continued to hold government meetings at the building. Though Minden is unincorporated, the groups meeting in this building have acted as local liaisons to Douglas County&#39;s government and have helped manage local government services. In addition, the building has continued to house a variety of social events, including concerts, movies, religious services, and basketball games.</p><br>
<p>The building was added to the National Register of Historic Places on August 4, 1983.</p><br>
<p>The Minden Inn is a historic hotel building located at 1594 Esmeralda Avenue in Minden, Nevada. Built from 1912 to 1916, the building was designed by prominent Nevada architect Frederic Joseph DeLongchamps in the Classical Revival style. The hotel was the largest commercial building in Minden and was operated by H. F. Dangberg, the founder of the town. The inn earned a reputation as "one of the finest small hotels on the West Coast" and was visited by a number of actors and celebrities who passed through Minden on the Virginia and Truckee Railroad. In addition, the hotel included a bar and gambling operations until 1987. The building now houses Douglas County offices.</p><br>
<p>The hotel was added to the National Register of Historic Places on August 6, 1986.</p><br>
<p>The Turtle-Flambeau Flowage is a 12,942 acre lake, located in Iron County, Wisconsin. It has a maximum depth of 50 feet. Fish include Musky, Panfish, Largemouth Bass, Smallmouth Bass, Northern Pike, Walleye and Sturgeon. The lake&#39;s water clarity is low.</p><br>
<h2>History</h2><br>
<p>The Turtle-Flambeau Flowage was created in 1926 when the Chippewa and Flambeau Improvement Company built a dam on the Flambeau River downstream from its confluence with the Turtle River. The dam flooded 16 natural lakes and formed an impoundment of approximately 14,000 acres.</p><br>
<p>The flowage was constructed as a reservoir to augment river flows and sustain hydroelectric plants operated downstream by electric utilities and paper mills. The dam also provided flood protection and created a unique recreational resource.</p><br>
<h2>Tourism</h2><br>
<p>The Turtle-Flambeau Flowage is a major destination of summer tourism. Visitors have access to the lake from four public boat landings. Camping, hunting, and fishing are also popular activities. The Turtle-Flambeau Scenic Waters Area offers 60 remote campsites accessible by water only. These sites are available year-round on a first-come, first-served basis. There is no camping fee, but camping on the flowage is restricted to designated sites.</p><br>
<p>Historically, many lakeside resorts have existed in the vicinity of the flowage. However, today much of the shoreline remains sparsely developed.</p><br>
<h2>Management</h2><br>
<p>Some lake management activities are undertaken by the Turtle-Flambeau Flowage & Trude Lake Property Owners Association, Inc.</p><br>
