<p>Cabin Ben is a historic log house at 115 Cullasaja Drive in Highlands, North Carolina. The house consists of two rectangular sections, joined at an offset. The smaller of the two sections houses a large living room, while the larger section houses the kitchen, dining, and bedroom areas. The house was designed by Clemson University professor of architecture Rudolph Edward Lee for a family friend, Miss Anne England, and was built in 1932 by Joe Webb, a locally prominent builder of log houses. It is a relatively unaltered example of Webb&#39;s work, having been designed to house relatively large family gatherings. It has remained in the hands of England descendants.</p><br>
<p>The house was listed on the National Register of Historic Places in 2003.</p><br>
<p>The 751-metre-high Gebaberg, also called the Hohe Geba or Die Geba, is the highest point of the Anterior Rhön  and lies in southern Thuringia in Germany.</p><br>
<h2>Location</h2><br>
<p>The mountain is located about 11 kilometres west of the county town of Meiningen.</p><br>
<p>In the south of the broad summit plateau lies the village of Geba, in the northe is the highest point of the mountain with a walking hut and cafe. At the southern foot of the massif, in the valley of the Herpf river are the villages of Wohlmuthausen, Helmershausen and Bettenhausen which, like the village of Seeba to the southeast, belong to the municipality of Rhönblick. On the eastern slopes of the Geba lies the village of Träbes with the sinkhole of Träbeser Loch and in the valley lie the villages of Stepfershausen and Herpf, the latter in the borough of Meiningen. North of the Geba is the Katzgrund valley with its villages Unterkatz and Oberkatz. In the northwest behind the Diesburg is the village of Aschenhausen.</p><br>
<h2>Description</h2><br>
<p>Also part of the extensive massif are the tops of Neidhardskopf (721 m) in the south, the Hohe Löhr (638 m) and the Diesburg (713 m) in the west.</p><br>
<p>At the edge of the wooded summit plateau there is an observation knoll with a panoramic view of the Bavarian, Hessian and Thuringian Rhön, the Thuringian Forest, the Haßbergen and the Hoher Meißner.</p><br>
<h2>History</h2><br>
<p>In 1867 the Duchy of Saxe-Meiningen had the first surveys carried out on the Geba, during which the first log cabin was built as protection from the weather. On 2 June 1897 the first Meininger Hut (Meininger Hütte) was inaugurated in the presence of Duke George II. The hut was later extended. In the decades that followed, the Geba developed into a popular destinations for walkers and holidaymakers looke for peace and relaxation, thanks to its good views.</p><br>
<p>From 1945 to 1962 the building was used by the Free German Youth (FDJ) as a youth hostel. Thereafter, the Soviet Army occupied the highest point of the summit plateau and built a radar station. The terrain was placed out of bounds and was no longer accessible to local people and visitors.</p><br>
<p>At the end of the 1960s, a local German firm built a barracks for the Soviet Army. In "House I" (today the Gebatreff) was an armoury, a political room for education, a dormitory for 120 soldiers, a kitchen, a dressing chamber, dining rooms and simple toilets and bathrooms. On 22 April 1991 the Soviet soldiers left and House 1 was gutted by ABM-forces.</p><br>
<p>In 1998 the Meiningen Hut was re-opened by the Meiningen branch of the Rhön Club on its historic site. It contains a lounge with a stove and a dormitory. In addition, in 1999 a Rhön cultural garden, 3 hectares in area, was laid out at the summit with a reconstruction of a Celtic village.</p><br>
<p>In the late 1990s the barracks were gradually converted and today they house the Bergstübchen cafe, an event hall, a club lounge, a training room, the Russian museum, Дружба ("Friendship") and an information point for the Geba Tourist Association (Fremdenverkehrsverein Geba e.V.).</p><br>
<p>On 28 August 2005 the Rhön Club inaugurated a metal table on the observation knoll with 40 direction indicators for places in the Rhön, the Werra valley and the Thuringian Forest.</p><br>
<p>Rhoenlandschaft-2004-04-12.jpgView of the Gleichbergen</p><br>
<p>Geba-2004-04-12.jpgCeltic village under construction</p><br>
<p>Herbstlicher Rhoenblick von der Geba 1.JPGRhönblick in the autumn</p><br>
<p>Herbstlicher Rhoenblick von der Geba 2.JPGRhönblick in the autumn</p><br>
<h2>Walks</h2><br>
<p>The following run over the Geba:</p><br>
<p>the Geba Way (Gebaweg), an Extra tour of the Hochrhöner</p><br>
<p>the Julius Greif circular walk with a stone monument</p><br>
<p>the Milseburg Way (HWO3)</p><br>
<p>the Rhön-Rennsteig Path, which links the Geba with Aschenhausen and Stepfershausen.</p><br>
<p>the Thüringian Rhön Path</p><br>
<p>The Hohe Schule, formerly also the Aalhauck, near Völkershausen in the Bavarian county of Rhön-Grabfeld is, at about, the second highest hill in the Eastern Rhön Foreland after the Wurmberg.</p><br>
<p>The area includes ramparts and finds from the Hallstatt culture and the Latene Culture, section of the Landwehr, and the Rhine-Weser Watershed.</p><br>
<h2>Geography</h2><br>
<p>The summit of Hohe Schule rises 1.8 kilometres east-southeast of the village church of Völkershausen (in the municipality of Willmars), 2.6 kilometres north-northwest of the church in Eußenhausen (part of Mellrichstadt) and 2.5 km (as the crow flies) south-southwest of the church of Hermannsfeld (part of Rhönblick). The boundary between the territories of Willmars in the west and Mellrichstadt in the east runs over the summit region from north to south. The western flank of the hill lies within the Rhön Biosphere Reserve. In addition the Rhine-Weser Watershed passes over the summit too. East of the hill rises the Ellenbach and, to the northwest is the source of the River Linz.</p><br>
<p>The Pleß is a mountain, in the county of Schmalkalden-Meiningen in the Salzungen Werra Highland in the German state of Thuringia.</p><br>
<h2>Location</h2><br>
<p>The Pleß is generally seen as the northeasternmost mountain of the Anterior Rhön,but is counted by the Bundesanstalt für Landeskunde as part of the adjacent natural region of the Salzung Werra Upland to the northeast. The Thurigian State Office for Geology and the Environment (Thüringer Landesanstalt für Umwelt und Geologie) sees it as part of the Rhön. Geologically it was clearly formed as part of the volcanism of the Rhön, but is surrounded by the bunter sandstone of the Werra Upland.</p><br>
<p>Among the nearest municipalities are Bad Salzungen to the north. Breitungen to the east-northeast, the nearby Rosa to the south and Urnshausen to the southwest. Seen from the Thuringian Forest which is somewhat further east it is on the left (east-southeast) next to the mountains of Baier, Dietrichsberg (Dietrich) and Öchsenberg (Öchsen).</p><br>
<h2>Description</h2><br>
<p>The Pleß is of basaltic volcanic origin.</p><br>
<p>At the summit of the Pleß is a viewing tower from which the mountains of the Thuringian Forest and the Rhön, the valley of the Werra and the castle of Wartburg can be seen.</p><br>
<h2>History</h2><br>
<p>The original name of the Pleß was the Bleßberg. However, because there were two Bleßbergs in the Duchy of Saxe-Meiningen, an "upland" Bleßberg in the vicinity of Eisfeld and this "lowland" one - which often led to confusion – the name was changed at the behest of Duke George II at the end of the 19th century to Pleßberg. A short time later, the suffix "-berg" was dropped.</p><br>
<p>As early as the 19th century the Pleßhaus (north of the summit) and a viewing tower were built. In East Germany the mountain was declared an out-of-bounds area as part of the Bad Salzungen Training Area which extended mainly to the north of the mountain. The Pleßhaus was used as accommodation for the soldiers. Later, a barracks was built on the Pleß, but it stood empty and slowly decayed. Even the viewing tower was demolished.</p><br>
<p>Keen locals began the preservation of the Pleßhaus. The new Pleßhaus was rebuilt at the Jägerstein. The inn there bears the name Seeblick today.</p><br>
<p>Following the gradually withdrawal of the Bundeswehr during the 1990s, it became possible to walk in the area again. In March 1996 the municipality of Breitungen purchased the area of the Pleßberg and has since had its own Hausberg. In the wake of that, some time later a new observation tower was built on the Pleß.</p><br>
<p>Pless.jpgThe Pleß seen from Dolmar</p><br>
<p>Pless-Rhoen.jpgView of the Pleß and Stoffelskuppe (left) from the south</p><br>
<p>Aussichtstum Pleß.jpgThe new viewing tower on the Pleß</p><br>
<p>Pleß-Rhön.JPGThe Pleß seen from the Thuringian Forest</p><br>
<p>The Dunnavant&#39;s Building is a historic commercial building in Huntsville, Alabama. It was built in 1905 by dry goods company Terry Brothers & Rogers. P. S. Dunnavant took control of the company in 1925, and the store remained in its downtown location until 1975. The third floor and roof were damaged in a fire in 1940. The ground floor on the Washington Street façade is framed by large brick piers with polished marble bases. Large display windows flank a recessed entry with a central column flush with the façade. All other windows are one-over-one sashes. A row of small, evenly spaced arched windows line the ground floor along the Clinton Avenue side. On the second floor façade there are two groups of four windows, each group sharing a stone sill. Third floor windows are smaller, and joined by brick arches. Windows along the Clinton Avenue side are similarly treated. The building is topped with a simple, denticulated cornice, with the roofline stepping down towards the rear of the building. The building was listed on the National Register of Historic Places in 1980.</p><br>
<p>Lake Maloye Miassovo  is located in Chelyabinsk Oblast on the east side of the Ural Mountains, 62 km west of Chelyabinsk and 10 km east of Miass. It partially adjoins Ilmen Nature Reserve.</p><br>
<p>The lake is of tectonic origin; a duct connects the lake to Lake Bolshoye Miassovo. The lake has extensive aquatic vegetation, with wetlands and wooded ridges along the shore. The bottom is mainly rocky, with silt in places. Inflow of water is from keys and small rivers.</p><br>
<p>Fish found in the lake include roach, perch, pike, ruff, tench, crucian carp, burbot, and whitefish.</p><br>
<p>The lake is popular for recreation because of the beautiful landscapes. Pine and mixed forest grow on the banks. There are rock outcrops in the form of stone ridges, slabs, boulders and stone deposits.</p><br>
<p>Near the lake there are archaeological sites. The ancient human settlement "Linden oxbow lake" (Russian: Липовая курья) was a haven of a small tribe of about 5,000 years ago. A total of about 30 prehistoric settlements have been found, with a variety of artifacts: pottery vases with ornaments, stone knives, and scrapers.</p><br>
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<p>The Johnson-Morris House is a historic house at 41 Upper Pike Creek Road in northern New Castle County, Delaware. The core of the main house is a fieldstone farmhouse built c. 1803; it has four bays across and is two stories tall. A two-story ell, extending west from this main block, was added not long afterward. The house remained the central point of a farm until 1937, when it was purchased by Hugh M. Morris, a judge on the bench of the United States District Court for the District of Delaware. Between 1937 and 1939, the house underwent a major expansion, adding large ells, and restyling the original with Colonial Revival features. An earlier Colonial Revival transformation funded by Morris is now part of White Clay Creek State Park, part of which abuts this property.</p><br>
<p>The house was listed on the National Register of Historic Places in 2011.</p><br>
<p>Quietdale  is a historic residence in Huntsville, Alabama. The house was built in 1854 for Caroline Moore Robinson, the widow of Madison County Sheriff William Robinson. It represents a shift in architecture from Neoclassical to more eclectic forms that would become prominent in the late 19th century. The main block of the house is rectangular, with an ell off the rear and a two-story porch following the ell. The hipped roof is truncated to form a rooftop deck. A two-story, three-room, servants&#39; quarters is connected to the house via the porch. Centered on the façade is a single-story hipped roof porch supported by six slender, octagonal columns with corbelled arches in the architraves. A similar porch extends along the west side of the house. 5 large six-over-six sash windows stretch across the second floor, while the side of the house has two windows centered between two chimneys, with another window outside of them. There were originally two separate staircases which led to the divided second floor, but they were combined and the second floor joined by second owner Erskine Mastin. The house was listed on the National Register of Historic Places in 1982.</p><br>
<p>Ou Kaapse Weg , numbered as route M64, is a mountain pass in the Cape Peninsula that connects the Southern Suburbs of Cape Town with the Fish Hoek Valley. It traverses the Steenberg mountains and passes through the Silvermine Nature Reserve. Ou Kaapse Weg is one of three routes to the Fish Hoek Valley: the others are Chapman&#39;s Peak Drive along the Atlantic coast and Main Road along the False Bay coast. Despite its name, the pass was only constructed in 1968, by the Divisional Council of the Cape.</p><br>
<p>Ou Kaapse Weg begins at a T-junction with Steenberg Road in Westlake, close to the southern end of the M3 expressway. It rapidly ascends the northern face of the Steenberg mountains, through two hairpin bends, to the summit at an elevation of 315 m. Near to the summit are entrance gates to the Silvermine Nature Reserve. The pass then descends along the valley of the Silvermine River, passing by Noordhoek to end at a junction with Kommetjie Road, which provides access to Kommetjie, Fish Hoek and other places in the Fish Hoek Valley.</p><br>
<p>In 2012 Ou Kaapse Weg suffered severe traffic congestion because it was used as an alternative route to avoid construction work on Main Road between Muizenberg and Fish Hoek.</p><br>
<p>Mauses Creek is a tributary of Mahoning Creek in Montour County, Pennsylvania, in the United States. It is approximately 5.9 mi long and flows through Liberty Township and Valley Township. Indian Creek is its only named tributary. The watershed of Mauses Creek has an area of 11.40 square miles. The main rock formations in the watershed are the Bloomsburg and Mifflintown Formation, the Wills Creek Formation, the Hamilton Group, and the Trimmers Rock Formation. Soil series in the watershed include the Berks-Weikert-Bedington series and the Clymer-Buchannnon-Norwich series.</p><br>
<p>Mauses Creek experiences siltation, organic enrichment, and low levels of dissolved oxygen. It is also contaminated by some organic compounds. The creek is crossed by six bridges.</p><br>
<p>In his book Trout Unlimited&#39;s Guide to Pennsylvania Limestone Streams, A. Joseph Armstrong describes Mauses Creek as "very similar to the upper portions of Kase and Sechler runs". It is inhabited by trout and chubs, as well as several other fish species.</p><br>
<h2>Course</h2><br>
<p>Mauses Creek begins in Liberty Township, near Mooresburg. It flows south for some distance before turning northeast, running parallel to railroad tracks for some distance before crossing Pennsylvania Route 642 and making an abrupt turn east. A short distance later, the creek exits Liberty Township. Upon leaving Liberty Township, the creek enters Valley Township. It continues east for a few miles, flowing parallel to Pennsylvania Route 642. The creek then turns northeast, away from the state route and it picks up the tributary Indian Creek after a short distance. It then turns southeast, flowing parallel to Pennsylvania Route 54. After some distance it crosses Pennsylvania Route 642 and passes the community of Mausdale. The creek reaches its confluence with Mahoning Creek in the southern edge of Valley Township.</p><br>
<p>Mauses Creek joins Mahoning Creek 3.00 mi upstream of its mouth.</p><br>
<h3>Tributaries</h3><br>
<p>The only named tributary of Mauses Creek is Indian Creek. It mainly flows in a north-south direction and joins Mauses Creek 1.20 mi upstream of its mouth. Indian Creek&#39;s watershed has an area of 1.92 square miles.</p><br>
<h2>Hydrology</h2><br>
<p>Most of Mauses Creek is considered by the Pennsylvania Department of Environmental Protection to be impaired. A few of its tributaries are also considered to be impaired, although most of them are not.</p><br>
<p>Mauses Creek experiences siltation and organic enrichment. It also has low levels of dissolved oxygen.</p><br>
<p>Chemicals such as trichloroethylene and 1,2-dichloroethene contaminate Mauses Creek in its lower reaches, near the MW Manufacturing Company site, 0.5 mi from the creek&#39;s mouth. These chemicals are not present further upstream.</p><br>
<p>The ten-year seven-day average minimum discharge of Mauses Creek is 63 gallons per minute.</p><br>
<h2>Geography and geology</h2><br>
<p>The lower reaches of Mauses Creek lie over rock of the Bloomsburg and Mifflintown Formation and the Wills Creek Formation, as do the creeks southern tributaries. Most of the rest of the creek is on rock of the Keyser and Tonoloway Formation. The creeks northern tributaries are over rock of the Hamilton Group and the Trimmers Rock Formation. The creek is not influenced by limestone.</p><br>
<p>Nearly all of the soil in the watershed of Mauses Creek is of the Berks-Weikert-Bedington soil series. However, the mouth of the creek and the upper reaches of some of its southernmost tributaries are over soil of the Clymer-Buchannnon-Norwich series.</p><br>
<p>Mauses Creek is between 10 ft and 15 ft wide.</p><br>
<h2>Watershed</h2><br>
<p>The watershed of Mahoning Creek has an area of 11.40 square miles. There is a strip of developed land in the creek. The area of developed land is mostly surrounded by agricultural land. There are areas of forested land in the watershed, but they are further away from the creek itself. A marshy area is located near the creek in its lower reaches.</p><br>
<p>Mauses Creek is close to Danville. The creek is in the Riverside United States Geological Survey Topographical Quadrangle.</p><br>
<h2>History</h2><br>
<p>Six surviving bridges have been built over Mauses Creek. One was built in 1915, two were built in 1963, one was built in 1975, and one was built in 1985.</p><br>
<p>A site known as the MW Manufacturing Company released pollution into Mauses Creek in the 20th century.</p><br>
<h2>Biology</h2><br>
<p>Although Mauses Creek is stocked, there are few trout in it. The creek does, however, have a large population of chubs. Additionally, darters, dace, minnows, and bass inhabit the creek. The waters of the creek are approved trout waters. Locals commonly fish there.</p><br>
<p>Mauses Creek is designated as a warmwater fishery and a migratory fishery.</p><br>
<p>There are no known endangered or threatened species in Mauses Creek.</p><br>
<p>Contamination from the MW Manufacturing Company site on Mauses Creek has a slightly adverse effect on the creek near the site, but no effect further downstream.</p><br>
<p>The Phelps–Jones House is a historic residence in Huntsville, Alabama. One of the oldest buildings in Alabama, it was built in 1818, shortly after the initial federal land sale in Madison County in 1809. Despite having many owners, the original character of the house has remained. The two-story house is built of brick laid in Flemish bond, and has Federal and Georgian details. The original block has a bedroom and parlor separated by a central hall, with a dining room in an ell to the northeast. Staircases in the hall and dining room led to three bedrooms on the second floor. In 1956, a porch in the crook of the ell was enclosed, adding a bathroom and small bedroom. Another porch off the rear of the dining room was enclosed and converted into a kitchen. Interior woodwork, including six mantels, is in provincial Federal style. The façade is five bays wide, with twelve-over-twelve sash windows on the ground floor and twelve-over-eight on the second. A narrow hipped roof porch covers the double front door; originally a wider porch covered a single door flanked by narrow sidelights and topped with a transom. The house was listed on the Alabama Register of Landmarks and Heritage in 1979 and the National Register of Historic Places in 1982.</p><br>
<p>The Everett Building is a historic commercial building in Huntsville, Alabama. Built in 1899, it represents the Commercial Brick style of the late 1800s and early 1900s that eschewed the applied decoration of the Victorian style. The two-story building is divided into five storefronts, although only the southernmost two have entrances today. The upper floor is divided by pilasters between tightly spaced, one-over-one sash windows. Decorative patterned reliefs sit below each window. The building is topped with a parapet that has a course of dentils between courses of stepped brick. The center part of the parapet is raised, and flanked by a short, capped column pieces. The northern bay is visually separated from the others by a pilaster stretching the entire height of the building, and was formerly left unpainted, suggesting it may have been built at another time. A covered, tree-lined alley separates the building from the Yarbrough Hotel to the north. The building was listed on the National Register of Historic Places in 1980.</p><br>
<p>The Randolph Street Church of Christ is a historic church in Huntsville, Alabama. It was built in 1887 in a Gothic Revival style similar to rural churches, but built of brick. Rather than a central entrance, the tower contains doors under pointed toplights on the sides, and a double lancet window joined under a pointed arch. Another set of lancets flanks the tower. On the corners of the façade and along the side walls are pilasters, dividing the sides into bays with one set of lancets each. The eaves of the gable are corbelled. Above the eaves, the tower is faced with tin, and each side has a pair of arched vents below a small gable. A modern spire and weather vane top the tower. The church sits half a block from Courthouse Square, adjacent to the rear of the Milligan Block. The church was listed on the National Register of Historic Places in 1980.</p><br>
<p>Psachna  is a small Greek town in Euboea, 16 km north of Chalcis. It is built in a small plain in the central-west part of the island. Psachna is the seat of Dirfys-Messapia municipality and the seat of Messapia regional unit. The town is also known for the campus of Technological Educational Institute of Chalcis and the football team Iraklis Psachna. Its population is 5,827 residents according to 2011 census.</p><br>
<h2>History</h2><br>
<p>The settlement of Psachna built from refugees after the sack of Chalcis in 1470 during the First Ottoman–Venetian War. During Ottoman occupation, it was a small village with few houses. After Greek independence, refugees from Samos were installed in Psachna, leading to the naming of a district of Psachna as "Samiotika". The population of Psachna was increased in the last century from the residents of the more mountainous villages such as Pyxaria, Vavoula, Apogremno, which moved in Psachna.</p><br>
<h2>Historical population</h2><br>
<h2>Description</h2><br>
<p>The campus of the Technological Educational Institute of Chalcis is located at Psachna. Near Psachna are found three monasteries, the monastery of Saint John Kalyvitis, the monastery of Panagia Makrymallis and the monastery of Panagia Gorgoepikoos. The two first of them were built during Byzantine period, destroyed in subsequent years and rebuilt. The third monastery is contemporary, built after 1960.</p><br>
<p>Psachna has the best medical facilities in the area. Among the patients it has diligently and discreetly treated over the years is a well-known NATO admiral.</p><br>
<p>Capitancillo  is a small, coral island near Bogo City, Cebu, Philippines. The island is a protected marine sanctuary, featuring three dive sites and a lighthouse.</p><br>
<h2>Location and geography</h2><br>
<p>Capitancillo is a small uninhabited island northeast of Cebu Island in the Visayan Sea. It is 10 km southeast of Tabogon and Bogo Island and just outside Bogo Bay, near Sea Turtle Resort Tabgon. Three areas around the island (the Ormoc Shoal, the Nuñez Shoal, and the southwest wall of Capitancillo) are recognized dive sites. Polambato Port, Nailon Wharf, Marangog Cove, and Odlot Hideaway all serve as jumping-off points to the island from Bogo, and the trip takes anywhere from fifteen to forty-five minutes. There are no stores or accommodations available on the island.</p><br>
<h2>History</h2><br>
<p>Legends surrounding the island state that Capitancillo was named after Captain Basillo, the captain of a Spanish trading vessel. According to the legends, Captain Basillo insulted a local datu, named Bugtopasan. Bugtopasan cursed Captain Basillo and put a spell on him, transforming the Captain&#39;s galleon into the island.</p><br>
<h2>Lighthouse</h2><br>
<p>The original lighthouse was listed in the Faros Españoles de Ultramar as one of 27 major lighthouses of the Philippines. The Capitancillo lighthouse was built in 1905, with the current white steel tower dating from the 1950s. The tower is 83 ft high and flashes three white lights every ten seconds. The lighthouse&#39;s designation is ARLHS PHI-079.</p><br>
<p>Calama was a colonia in the Roman province of Numidia situated where Guelma in Algeria now stands.</p><br>
<p>G. Mokhtar places it just within the Roman province of Africa Proconsularis, to the east of Numidia, but it is generally believed to have been in Numidia, a province created probably in 198–199.</p><br>
<h2>History</h2><br>
<p>Calama was founded by the Phoenicians and called Malaca (meaning "salt"). This toponym is also the etymological root of Málaga in Spain. Malaca was situated in the Berber kingdom of Numidia. When this area later came under Roman rule, the city was renamed Calama.</p><br>
<p>Whether Calama is identical with the town of Suthul which the Roman propraetor Aulus Postumius Albinus Magnus unsuccessfully tried to take in 110 BC, (cf. Battle of Suthul) is disputed, with some denying and others cautiously affirming.</p><br>
<p>In the 1st century AD, Calama, then part of the Roman province of Numidia, became a major urban centre. It was given the rank of a Roman municipium as early as Hadrian, and of a colonia later. The city was sponsored by Vibia Aurelia Sabina, sister of the Emperor Commodus (late 2nd century). Calama was, with Setifis (Setif) and Hippo Regius (Annaba), one of the granaries of Rome in the 2nd and 3rd centuries AD. Under Septimius Severus, Calama became one of the most prosperous in the Roman empire, with thermae and a huge theatre.</p><br>
<p>Calama became a Christian bishopric, four of whose bishops are named in extant documents:</p><br>
<p>Donatus (not to be confused with Donatus Magnus) was accused in a council held in 305 of having handed over the sacred scriptures during the Decian persecution</p><br>
<p>Megalius gave episcopal ordination to Saint Augustine in 395 and died in 397</p><br>
<p>Saint Possidius, elected in the year of Megalius&#39;s death, took an active part in the joint Conference of Carthage (411) with Donatist bishops</p><br>
<p>Quodvultdeus was one of the Catholic bishops whom Huneric summoned to Carthage in 484 and then exiled.Pius Bonifacius Gams, Leipzig 1931, p. 464</p><br>
<p>Possidius wrote the first biography of Augustine, in which he lets it be known that he himself was one of the clergy of Augustines monastery when he was appointed bishop of Calama. When Calama fell into the hands of the Vandal king Genseric in 429, Possidius took refuge with Augustine within the walled city of Hippo Regius. He was present at Augustines death in 430.</p><br>
<p>No longer a residential bishopric, Calama is today listed by the Catholic Church as a titular see.</p><br>
<p>The invading Vandals captured and partially destroyed Calama and defeated Count Bonifacius near the city in 431.</p><br>
<p>After the conquest of Numidia by the Byzantine Empire, Solomon (a general of Justinian I) built a fortress there between 539 and 554. Calama&#39;s population was fully Christian in the 6th and 7th century.</p><br>
<p>With the spread of Islam, Byzantine rule of Calama ended by around the 11th century (see Guelma).</p><br>
<h3>Archeological remains</h3><br>
<p>Theatre. It is difficult to reconstruct the plan and general appearance of the Roman theatre. The only other important monument discovered are the public baths. The theatre was built in the first or second year of the 3rd century AD through the generosity of a certain Annia Aelia Restituta, who spent 400,000 sesterces on it. It was restored, indeed virtually rebuilt, from 1902 to 1918, after having served as a quarry. It is on a slope and measures 58.05 m in width. It was built with a rubble core revetted with ashlar. The tiers of seats had virtually all disappeared; they must have numbered 10 in the lower zone and 12 in the second. The orchestra was paved in marble. Behind the stage, which was flanked by two rectangular chambers, a portico with columns formed a facade.</p><br>
<p>Baths. The public Roman baths were built of rubble and revetted with ashlar and brick. These "thermae" may date as early as the 2nd century AD. Only one large rectangular chamber (22 x 14 m), undoubtedly the tepidarium, can be described; it gave onto other rooms and onto the exterior by 11 passages. These baths were included within the Byzantine fortress, no doubt built on an earlier enclosure and defended by 13 towers. It measured 278 x 219 m.</p><br>
<p>Forum. The existence of a forum is attested by a single inscription. There are also remains of arcades, a small shrine of Neptune, cisterns and, outside the town, a Christian church. In 1953 a hoard of 7,499 coins was discovered; virtually all of them came from the mint at Rome; the most recent dated to the beginning of AD 257. Presumably the hoard was buried because of local disturbances. Most of the ancient objects recovered at Calama and from the region are preserved in the Guelma Museum.</p><br>
<p>Citadel and walls. Among its ruins are also a Byzantine citadel and walls built by the Byzantine patricius Solomon during the Byzantine reoccupation.</p><br>
<p>The Borden Milk Plant, now the home of the Fayetteville-Lincoln County Museum, is a historic dairy processing plant in Fayetteville, Tennessee.</p><br>
<h2>History</h2><br>
<p>The Borden Milk Plant was built by the Borden Company in 1927 to process raw milk into butter and powdered milk. It was among the earliest industrial facilities to be established by a major USA company in the former Confederacy in the years after the American Civil War.</p><br>
<p>The facility was important to the economy of Lincoln County and the surrounding region, particularly during the Great Depression, when it provided the only source of cash income for the area&#39;s farmers. In its first month of business, it paid $25,000 to the farmers who supplied raw milk. At its peak of operation, it had 75 employees and obtained milk from over 1,200 dairy farmers in the area. Local hog farmers used whey from the plant (a byproduct of milk processing) as a supplementary feed for their hogs.</p><br>
<p>In its later years, the plant produced cottage cheese from skimmed milk. During World War II, it supplied dried eggs and dried milk to the USA military.</p><br>
<p>The milk processing plant closed in 1962. In 1988 the facility was listed on the National Register of Historic Places as the "Borden Powdered Milk Plant".</p><br>
<h2>Museum</h2><br>
<p>The Fayetteville-Lincoln County Museum, which is housed in the former milk plant, has 33,000 ft2 of exhibit space. The history of agriculture in the local area is a major focus of the museum. Other exhibits include a large collection of Native American artifacts, an electric train display, and items related to the military career of USA Admiral Frank Kelso, a native of Fayetteville.</p><br>
<p>Lake Kuyucuk  is a small shallow lake located in Arpaçay district of Kars Province in the Eastern Anatolia Region of Turkey. It has an area of 245 hectare and a maximum depth at 13 m. The lake area is an internationally recognized Ramsar site, important for its ornithofauna, and a tourist wildlife reserve.</p><br>
<h2>Geology</h2><br>
<p>The Kalkankale Formation, consisting of old sandstone, mudstone and claystone dating back to early Pliocene period, underlies wide areas at Lake Kuyucuk and the surrounding landscape, and forms the flat and low-sloped terrain of the region. Elevations north of the lake are formed by agglomerate, tuff and andesite of early Pliocene old Kura volcanic rocks while the southwestern elevations are formed by tuff, andesite, pearlite, pumice and obsidian of Dumanlıdağ pyroclastic rocks.</p><br>
<h2>Topography</h2><br>
<p>Büyükalamet Heights 1,676 m, Küçükalamet Heights 1,657 m, Kızılgüney Heights 1,646 m and Uzungüney Heights 1,660 m in the north, Alaca Heights 1,693 m in the west and Cadalı Heights 1,772 m, Yumru Heights 1,656 m and Mevzili Heights 1,655 m in the southwest are the elevations around the lake making up the landscape&#39;s topography.</p><br>
<h2>Flora</h2><br>
<p>At an elevation of 1,627 m, the lake region has two ecosystems, steppe and wetland. The wetland flora are free-floating aquatic plants from the duckweed family (Lemna), common reed (Phragmites australis) and rushes (Juncus) while the steppe flora are shrubs and herbs (Astragalus, Onobrychis), vetches (Vicia), daisy (Artemisia), common dandelion (Taraxacum officinale) and alsike clover (Trifolium hybridum).</p><br>
<p>The globally threatened plant species grass (Elymus sosnowskyi), which is endemic to Turkey, grows here.</p><br>
<h2>Fauna</h2><br>
<p>Lake Kuyucuk is a wetland site for 232 bird species, and is a Ramsar site designated as of international importance in 2009, stretching over an area of 416 hectare. It is Turkey&#39;s thirteenth Ramsar site, and the first one in eastern Turkey. The lake has great ornithological importance, being on the African-Eurasian flyway of migratory birds. It has been recognized by BirdLife International as an Important Bird Area in 2004. In the fall, more than 40,000 birds stop over at the lake. An artificial islet on the lake was formed in 2009 to provide a safe breeding place for bird species and to help protect them from predators.</p><br>
<p>The Ramsar site harbors bird species such as ruddy shelduck (Tadorna ferruginea), the globally endangered white-headed duck (Oxyura leucocephala), red-breasted goose (Branta ruficollis), velvet scoter (Melanitta fusca), western marsh harrier (Circus aeruginosus), common crane (Grus grus), black-winged stilt (Himantopus himantopus), Eurasian coot (Fulica atra), black-necked grebe (Podiceps nigricollis), common starling (Sturnus vulgaris) and greylag goose (Anser anser).</p><br>
<p>The Kuzey Doğa, a Turkish non-governmental organization for nature conservation, operates a station at the lake, which carries out birdwatching, bird ringing and bird counting. Lake Kuyucuk hosts the country&#39;s ever first bird ringing station, where over 22,500 birds of 170 species were ringed until January 2010. Bird ringing is done around April 1. In 2011, a birdwatching tower was built at the lake. In September 2004, over 20,000 ruddy shelduck, which makes out almost 12% of the world population, were observed on the lake in just one day.</p><br>
<p>Other notable fauna found around the lake are the mammal species red fox (Vulpes vulpes), Nehring&#39;s blind mole rat (Spalax nehringi), southern vole (Microtus levis) and marbled polecat (Vormela peregusna), the amphibians European green toad (Bufo viridis) and marsh frog (Pelophylax ridibundus) as well as the reptile species sand lizard (Lacerta agilis).</p><br>
<p>The highly acidic water of the lake does not support fish species.</p><br>
<h2>Climate</h2><br>
<p>The Lake Kuyucuk and its surroundings are situated in the coldest zone of Eastern Anatolia characterized with harsh continental climate. Winters are long and very cold, summers are moderate, even coolish. Maximum precipation is observed in May while in January precipation is at minimum.</p><br>
<h2>Wildlife endangered</h2><br>
<p>By January 2014, it was reported by Kuzey Doğa that the wildlife at the lake is endangered. The lake&#39;s water level decreased down to 2 -. That resulted in connecting of the artificial breeding islet with the lake shore at some places, which brings the birds in danger by predators. Moreover, the vegetation on the islet was destroyed as it was used by the local herdsmen as fodder for their livestock. The negative change of the ecosystem was caused mostly by drought arisen from insufficient water inflow and excessive extraction of groundwater in local wells drilled by the villagers. In addition, the creek feeding the lake is used as watering trough for livestock by blocking their flow.</p><br>
<p>The Kuzey Doğa proposed to set up a planning for water supply in the basin and to immediately reform the islet by digging a ditch around.</p><br>
<h2>Tourism</h2><br>
<p>The European Destinations of Excellence (EDEN) of the European Commission has listed Lake Kuyucuk as a notable tourist wildlife reserve since 2009. In 2012, a tourism center was built at the lake to serve for ecotourism. Since 2011, an annual two-day birdwatching festival is held in mid June.</p><br>
<p>The nearest populated place is Kuyucuk village, 1 km west of the lake. Until 1920, the village was inhabited by Molokans, members of a Christian sect. Later, Karapapaks, a Turkic-speaking sub-ethnic group of Azerbaijanis, settled in the village. A village school building, built by Molokans in 1907, is still intact. From the 1909-built three-story Russian orthodox church, only the first floor has survived. Other buildings, preserved from the Molokan times, are the village chambers.</p><br>
<p>Nature tourists and birdwatchers come to Lake Kuyucuk between the beginning of spring and the end of fall. The site is also visited by students of local schools and colleges on special days like World Biodiversity Day, World Environment Day, International Migratory Bird Day and Birdwatching Day.</p><br>
<p>The ruined medieval Armenian city-site Ani and the ruins of an 11th-century Shaddadids mosque, the Manucehr mosque (Menucehr camii) within the site of Ani, are notable tourist attractions in the vicinity.</p><br>
<p>Lake Çıldır is another tourist destination in the region.</p><br>
<h2>Access</h2><br>
<p>Lake Kuyucuk is accessible through the state road, which crosses over the northern part of the lake. It is about 40 km northeast of Kars and 15 km west of Akyaka, Kars. The road through Kuyucuk village is used to get to the lake.</p><br>
<p>Greenlawn  is a historic residence between Meridianville and Huntsville, Alabama. The house was built in 1849–50 by William Otey, replacing a log house built by his father in the early 1810s. Following William and his wife&#39;s deaths, the house was taken over by one of their granddaughters in 1907. Around 1925, the original Italianate portico was replaced with the current Greek Revival entrance, and a northern wing was added. The house fell vacant in 1963 and was later restored, now sitting at the entrance to a subdivision of the same name.</p><br>
<p>The house has a two story main block with a single story portion to the rear. The façade is dominated by a tetrastyle portico with Doric order columns. The double front door is flanked by sidelights and topped with a rectangular transom. Two chimneys in the gable roof ends are unusual in that they are exposed below the pediment, but pass behind the tympanum before exiting the top of the roof. The shed roof of the northern addition is hidden from the front by a wooden parapet. The interior is laid out with a central hall, divided into an entry foyer and rear stairhall, with two rooms to either side. The northern two rooms are separated by a narrow hall leading to a roofed porch. The parlor and dining room on the southern side are divided by a triple-leaf folding door. A hall and two bedrooms occupy the second floor.</p><br>
<p>The house was listed on the Alabama Register of Landmarks and Heritage in 1979 and the National Register of Historic Places in 1982.</p><br>
<p>Lake Crescent is a man-made reservoir located in the eastern side of the Midlands region of Tasmania, Australia, approximately 100 km north of Hobart.</p><br>
<p>Lake Crescent is the main home for the golden galaxias Galaxias auratus. Carp, Cyprinus carpio, were discovered in the lake in 1995, but were eradicated using innovative techniqes. Ramsar is an internationally significant wetland game reserve. The Short Fin Freshwater Eel (Anguilla australis) used to migrate to Lake Crescent from the ocean. However its movement has been impounded by dams on the Derwent River, and mesh screens on the Clyde River to limit the movement of carp. The Inland Fishers Service has been stocking elvers into the lake to sustain a commercial eel fishery. Other fish that are stocked and fished from the lake are brown trout and rainbow trout.</p><br>
<p>There is one boatramp into the lake accessed from Lake Crescent Road.</p><br>
<p>The Interlaken Waste Transfer Station is on Dennistoun Rd.</p><br>
<p>Meriden Town Hall is a historic municipal building at 110 Main Street in the Meriden village of Plainfield, New Hampshire. It is a two story wood frame structure, built in 1895. Its main facade is three bays wide, with double leaf doors sheltered by a gable-roof porch. Its principal exterior alterations since construction are the addition of the front porch in 1901, and the addition of a handicapped access ramp aod door to one of the side window bays in 1995.</p><br>
<p>The building is the only purpose-built town hall building in Plainfield, whose government is divided between Plainfield village (where Plainfield Town Hall is located) and Meriden. This town hall was built after the previous meeting house (built 1797), used for both religious and civic functions, was destroyed by fire in 1894.</p><br>
<p>The building was listed on the National Register of Historic Places in 1998.</p><br>
<p>The Mothers and Daughters Club House is a historic social club building on Main Street  in Plainfield, New Hampshire. It is a single story wood frame structure, five bays wide and one deep, with a pyramidal hipped roof. A small woodshed is attached to the east  end of the building, and there is a trellised front porch, added shortly after the building&#39;s construction. The building was designed by noted New Yorkc City architect Charles A. Platt and built in 1901; it is one of the oldest clubhouses for women in the country. The social club for which it was built was part of a social movement involving a renaissance of handicraft, in this instance predominantly involved in the creation of hooked rugs.</p><br>
<p>The building was listed on the National Register of Historic Places in 1982.</p><br>
<p>The Dorchester South Burying Ground is a historic graveyard on Dorchester Avenue in the Dorchester neighborhood of Boston, Massachusetts. Established in 1814, it is the second oldest cemetery in Dorchester, after the North Burying Ground. It is a roughly 2 acre parcel on the west side of Dorchester Avenue, north of Dorchester Lower Mills. A paved roadway provides circulation around the perimeter of the property. There is some evidence that the cemetery was formally terraced, due to the sloping terrain, but there is no evidence of curbing that might have been used for this purpose. One of the cemetery&#39;s most prominent features is a line of granite tombs along the southern boundary.</p><br>
<p>The cemetery was listed on the National Register of Historic Places in 2014.</p><br>
<p>Fort Loudoun was a historic fortification of the French and Indian War, located in what is now Winchester, Virginia. The fort was built between 1756 and 1758 under the supervision of George Washington, then a colonel in the militia of the British Province of Virginia. It was named for John Campbell, 4th Earl of Loudoun, who commanded the British forces in North America for a time during the war. Washington and his militia regiment were headquartered at the fort for two years. The fort was a roughly square bastioned earthworks, whose extent spread across where North Loudoun Street runs.</p><br>
<p>The property at 419 North Loudoun encompasses the historic heart of the fort, including a well dating to the fort&#39;s construction, and a portion of its northwest bastion. This area has been listed on the National Register of Historic Places. This property is now owned by the non-profit French and Indian War Foundation.</p><br>
<p>The Capt. Goodgame House is a historic house on Arkansas Highway 128 in Holly Springs, Arkansas. Built in 1918, this single story wood frame house is an unusual late and high quality example of a vernacular style of house architecture more typically seen in 19th century construction in the area. It has a gable roof, and is clad in novelty siding. A porch extends across the front facade, supported by plain chamfered posts. The gable ends of the roof are extended, with full pediments, and the door and window surrounds are more elaborate than are typically seen in the area. The interior of the house follows a standard central hall plan, but the detailing is again of a particularly high quality.</p><br>
<p>The house was listed on the National Register of Historic Places in 1983.</p><br>
<p>The Ed Knight House is a historic house near Pine Grove, a rural community in Dallas County, Arkansas. It is located on County Road 275 off Arkansas Highway 128. In appearance it resembles a double pen house, a narrow and wide structure with a gable roof. Its oldest portion is a dog trot log structure built c. 1880, after which the central passageway was enclosed and an ell added to the south end. This was then sheathed in horizontal weatherboarding. The front facade has a hip-roof porch extending across its width, supported by six turned posts, with jigsaw-cut brackets. The Knights were a prominent local family who settled the area in the 1840s.</p><br>
<p>The house was listed on the National Register of Historic Places in 1983.</p><br>
<p>Hampton Springs Cemetery is a cemetery in rural Dallas County, Arkansas, at the junction of county roads 425 and 427, near the city of Carthage. The cemetery is divided into two sections, one in which traditional European grave markers predominate, and another section in which graves are marked by a local adaptation of African burial customs. This African-American section of the cemetery is said to have been in use since the late 19th century, although its oldest identified grave is dated 1916. Most of its estimated 128 marked graves are denoted by informal means, including small bushes, ceramic objects, metal pipes, wooden stakes, offering vessels such as glass jars and bowls, and even a kerosene lamp. This section of the cemetery has been listed on the National Register of Historic Places as an important regional example of traditional African burial practices.</p><br>
<p>The George W. Mallett House is a historic house in Princeton, Arkansas, the first county seat of Dallas County. Built c. 1853 by George W. Mallett, one of the county&#39;s first settlers, it is one of three surviving pre-Civil War houses in the county, and the only one in Princeton. The house was originally built as a dog trot; the breezeway was enclosed around the turn of the 20th century, giving the house its present exterior appearance of a central hall structure. A hip roof covers the original portion of the house, while a gable covers a two-room ell added to the rear . A shed-roof porch extends across the width of the main facade, supported by chamfered posts.</p><br>
<p>The house was listed on the National Register of Historic Places in 1983.</p><br>
<p>The Marathon Oil Service Station is a historic automotive service facility at the southeast corner of East 2nd and Spring Streets in downtown Fordyce, Arkansas. It is a single story building constructed out of red and buff brick, with an auto canopy covered in a tile roof. The main facade of the building has a parapet which conceals a barrel roof. The building is divided into two functional bays, an office to the left and a garage bay to the right. The canopy extends in front of the left bay, and is supported by a single brick column, in which there is an original Marathon Oil logo. The building is a well-preserved example of a 1920s service station.</p><br>
<p>The station was listed on the National Register of Historic Places in 1992.</p><br>
<p>The Newport Downtown Historic District encompasses the 19th century heart of Newport, New Hampshire, the county seat of Sullivan County. The district includes the major commercial and civic  buildings which line Main Street between Depot Street and the Sugar River. The district was listed on the National Register of Historic Places in 1985.</p><br>
<p>Although Newport was settled in 1765, its current center began to take shape with the construction of the Croydon Turnpike, along what is now Main Street. The area was soon lined with services for travelers. The oldest commercial building in the district, the Eagle Block at 64 Main Street, was built in 1825-26; it is a three story Federal-style brick building. The town gained in importance when Sullivan County was set off from Cheshire County in 1826, resulting in the construction of the records office, jail, and the first courthouse, all brick Federal-style buildings. on the east side of Main Street. The courthouse (now used for other purposes) stands on a hill set well back from Main Street.</p><br>
<p>The west side of Main Street became the locus for commercial development, and now sports a series of buildings mostly built before 1930, anchored at one end by a modern state liquor store, and at the other end by a c. 1930 Worcester Lunch Car Company diner, which abuts the Eagle Block. The dominant feature of the east side is now the Newport Opera House building, which was designed by Hira R. Beckwith to serve as the courthouse and town hall, and replaced an 1872 building destroyed by a major fire. This building is now used mainly as a performing venue; the municipal offices are now located just outside the district on Sunapee Street. Also notable on the east side is the Isaac Reed House, one of the last private residences built in the area, and a particularly fine example of Italianate and Second Empire styling.</p><br>
<p>Middle Branch Chillisquaque Creek is a tributary of Chillisquaque Creek in Columbia County and Montour County, in Pennsylvania, in the United States. It is approximately 5.2 mi long and flows through Madison Township in Columbia County and Anthony and Derry Townships in Montour County. The creek&#39;s watershed has an area of 9.64 square miles. There are 14.35 mi of streams in the watershed. Lake Chillisquaque is also in the creek. There are 122 features classified as "disturbances" on Middle Branch Chillisquaque Creek. Two bridges more than 20 ft long cross the creek.</p><br>
<h2>Course</h2><br>
<p>Middle Branch Chillisquaque Creek begins in a valley in western Madison Township, Columbia County. It then exits Anthony Township and enters Derry Township, Montour County. In Derry Township, the creek almost immediately meets East Branch Chillisquaque Creek to form Chillisquaque Creek.</p><br>
<p>Middle Branch Chillisquaque Creek joins Chillisquaque Creek 19.96 mi upstream of its mouth.</p><br>
<h2>Hydrology</h2><br>
<p>Middle Branch Chillisquaque Creek is ranked 6th in priority on the 305B Stream Listings in the watershed of Chillisquaque Creek. It experiences siltation and has been subjected to hydromodifcation and flow alterations.</p><br>
<p>The water temperature of Middle Branch Chillisquaque Creek ranges from approximately 0 to 22 C.</p><br>
<p>The concentration of alkalinity in Middle Branch Chillisquaque Creek ranges from under 10 to over 70 milligrams per liter. The concentrations of nitrates and phosphates are both high.</p><br>
<h2>Geology and geography</h2><br>
<p>The depth of Middle Branch Chillisquaque Creek near Pennsylvania Route 44 typically ranges between a few inches and a foot (30 centimeters), but is occasionally over 20 in.</p><br>
<p>There are 122 features classified as "disturbances" on Middle Branch Chillisquaque Creek. 96 of these (78.7 percent) are erosion sites, 45 of which are on the creeks right bank and 51 of which are on the creeks left bank. 14 of the "disturbances" are gravel bars, 7 are bridges, 3 are riprap, and 2 are pipes.</p><br>
<p>There are nearly 30 stream banks on East Branch Chillisquaque Creek that area between 0 ft and 50 ft long. Slightly more than 20 are less than 6 ft high, 5 are 6 to 9 ft high, and approximately two are over 9 ft high. There are slightly over 30 banks on the creek that are 51 to 100 ft long. Between 15 and 20 are under 6 ft high, slightly more than 10 are 6 to 9 ft high, and approximately three are over 9 ft high. The creek has 25 banks that are 101 to 250 ft long. Of these, there are approximately equal numbers of banks less than 6 ft high and 6 to 9 ft high and none higher than 9 ft.</p><br>
<p>There are several stream banks on East Branch Chillisquaque Creek that are between 251 ft and 500 ft. Five are less than 6 ft high and two are over 6 ft hingh. The creek also has several banks over 500 ft long, all of which are less than 6 ft high.</p><br>
<p>The streambed of Middle Branch Chillisquaque Creek is publicly owned. The elevation of the creek near its mouth is 522 ft above sea level. Near its source, the creek&#39;s elevation is between 860 ft and 880 ft.</p><br>
<h2>Watershed</h2><br>
<p>The watershed of Middle Branch Chillisquaque Creek has an area of 6.94 square miles. There are 14.35 mi of streams in the watershed of Middle Branch Chillisquaque Creek. 12.86 mi, or 89.6 percent, are classified as "not attaining".</p><br>
<p>Lake Chillisquaque is a reservoir located on Middle Branch Chillisquaque Creek and is the largest lake in Montour County. The lake is dammed by an earth-fill dam that is 2,000 ft long and 54 ft high.</p><br>
<p>Middle Branch Chillisqauque Creek is the most significant tributary of Lake Chillisqauque.</p><br>
<h2>History, recreation, and etymology</h2><br>
<p>Lake Chillisquaque was created on Middle Branch Chillisquaque Creek in 1972. Its original purpose was as a supply of cooling water for a nearby power plant. Two bridges more than 20 ft long cross the creek. One was built in 1923 and is 43.0 ft long and the other was built in 1932 and is 28.9 ft long. Both bridges are made of concrete.</p><br>
<p>The Chillisquagi Trail in the Montour Preserve crosses Middle Branch Chillisquaque Creek.</p><br>
<p>The word chillisquaque in Middle Branch Chillisquaque Creek&#39;s name comes from either the Native American word chilisuagi, which refers to a place commonly visited by snowbirds (specifically, a "place frequented by snowbirds") or the Native American word for "frozen duck".</p><br>
<h2>Biology</h2><br>
<p>Lake Chillisquaque is stocked by the Pennsylvania Fish and Boat Commission. Middle Branch Chillisquaque Creek is designated as a warmwater fishery.</p><br>
<p>The Struve-Hay Building is a historic commercial building in Huntsville, Alabama. Built in 1900, it represents a transition between Victorian architecture style and the less ornamented Commercial Brick style. The building was originally two stories with a three-story tower on the corner, but the second story of the Jefferson Street façade was removed in 1955. Previously consisting of two storefronts, the Jefferson Street side was later combined into one, with a recessed central entrance flanked by pilasters and two large single-pane fixed windows on either side. This portion of the building is also painted white with green accents, rather than the red with unpainted stone accents of the remainder of the building, providing additional visual separation. The corner and first bay of either side are adorned with stone pilasters with capitals supporting a stone course that wraps around the building. The tower has a single one-over-one sash window on each face of the second floor, with a pair of small arched windows on the third. It is topped with a pyramidal roof and ball finial. Along Holmes Avenue, the first floor has no windows, while the second floor has a pair of one-over-one windows per bay. The building is topped with a bracketed pressed metal cornice. The roof on the end of the building on the Holmes side steps down to a separate unit, featuring a Romanesque Revival arched entryway below a bay window. The building was listed on the National Register of Historic Places in 1980.</p><br>
<p>Larymna  is a port town in Phthiotis, Greece. It is situated on the North Euboean Gulf. Since the 2011 local government reform, it is a part of the municipality Lokroi, of which it is a community. Larymna took its name from the ancient Boeotian port town Larymna, which was situated at the same place.</p><br>
<h2>History</h2><br>
<p>Larymna was ancient Locrian city. The city had been also existed a harbour of Thebes, where Thebes was in apogee, during 4th century B.C. The modern years, Larymna was a small village known also with the name Kastri. The name Kastri derives from the well-kept ancient wall in the coast. Larymna developed after the foundation of mining and metallurgical industry LARCO, opposite Larymna&#39;s port.</p><br>
<h3>Historical population</h3><br>
<p>The James Neal House is a historic house at 74 Deer Street in Portsmouth, New Hampshire. Built about 1830, it is distinctive as the only brick house to be built in the Deer Street area, and one of the last Federal style houses to be built in the city. It was listed on the National Register of Historic Places in 1972.</p><br>
<h2>Description and history</h2><br>
<p>The James Neal House stands in The Hill, a cluster of closely spaced historic houses bounded on the north by Deer Street and the east by High Street at the northern edge of downtown Portsmouth. This grouping was created by a road widening project from houses originally located on or near Deer Street. This house is a three-story brick structure, oriented facing west on the south side of Deer Street. The side facing the street is two bays wide, while the main facade is five bays wide, with a center entrance topped by a Federal style fanlight. The interior is finished in largely original transitional Federal-Greek Revival styling. It has a modestly Federal central stairway, and original fireplace surrounds.</p><br>
<p>The house was built about 1830-32 by James Neal, a local merchant. It is one of the last known examples of the Federal style built in the city. It is also unusual for its sophistication in what was then a residential area away from most of the city&#39;s merchant houses.</p><br>
<p>The Newington Center Historic District encompasses the historic civic heart of Newington, New Hampshire. It consists of a section of Nimble Hill Road between its junction with Little Bay Road, and a gate at the southern end marking the start of territory formerly associated with Pease Air Force Base . This area includes the town common, laid out in 1640, a cluster of civic buildings, and several private residences, as well as remnants of the state&#39;s oldest town forest. The district was listed on the National Register of Historic Places in 1987</p><br>
<h2>Description and history</h2><br>
<p>The town of Newington was originally settled in the 17th century as part of Dover. It was set off as a separate parish in 1712, and incorporated as a separate town in 1713. Its historic town center&#39;s origins date to 1640, when common land was set aside by the town. Some of this became the town center area, and a larger part (eventually reaching more than 100 acre in size) was at some point designated as the town forest.</p><br>
<p>The town center is clustered along a section of Nimble Hill Road, a historic north-south route between Dover and Portsmouth, and is also passed just to the north by a historic alignment of the Old Boston Post Road, connecting Boston, Massachusetts, to points in what is now Maine. The north-south road was truncated at its southern end by the construction of Pease Air Force Base in the 1950s, which also greatly reduced the town forests size. One of the centers focal points is the Congregational Church, a structure built in 1712 and extensively altered in 1835, giving it its present Greek Revival appearance.</p><br>
<p>The Newmarket Industrial and Commercial Historic District encompasses the heart of a distinctive 19th century mill town, Newmarket, New Hampshire. Its mill complex is regionally distinctive for its extensive use of stone from an early date, and the town is relatively well-preserved due to a significant economic decline after the mills closed in 1920. The district was listed on the National Register of Historic Places in 1980. The Stone School, listed in 1978, is a contributing resource.</p><br>
<h2>Description and history</h2><br>
<p>The town of Newmarket was incorporated in 1737, and was initially a shipping center, based on the Lamprey River, a tributary of the Piscataqua River. In the early 19th century, the power of the Lamprey River was harnessed by textile manufacturing businesses, which fueled the communitys growth into the early 20th century. That industry then declined, leaving a distinctive architectural legacy in New Hampshires Seacoast Region. The most notable aspects of the town&#39;s buildings is the use of stone, in contrast to other mill towns of southern New England, which predominantly used brick. The use of stone was not limited to the mills themselves: the historic district also has examples of stone houses, churches, and schools.</p><br>
<p>The historic district extends along Main Street (New Hampshire Route 108) between Gerry Street and Elm Street, Exeter between Gerry and Main, Nichols and Central streets, and a number of smaller adjacent streets between Main Street and Granite and Spring streets. Its principal eastern boundary is the Lamprey River, along which the surviving mill buildings are arrayed. Commercial buildings are mainly located across Main Street from the mills, with residential housing on side streets. A cluster of town buildings and a church are located at the junction of South Main Street and Beech Street Extension. The town hall is a handsome Greek Revival brick building constructed in 1847.</p><br>
<p>The Nichols Memorial Library is a historic library building on Main Street in Kingston, New Hampshire, United States. Built in 1898, it is distinctive statewide as the only local library building exhibiting Shingle style and Richardsonian Romanesque features. It was used as the town library until 2012, and now houses the town&#39;s research collection and archives. The building was listed on the National Register of Historic Places in 1981.</p><br>
<h2>Description and history</h2><br>
<p>The former Nichols Memorial Library building stands in the village center of Kingston, at the eastern corner of Main and Depot Streets. The building is a single-story irregular stone structure with a red slate hip roof, and a fieldstone chimney at one side. A semicircular section projects from the front facade, just to the right of the main entrance, which is sheltered under an eyebrow-gabled portico. Window openings are generally square or rectangular and vary in size. The largest of them have stained glass transoms depicting the marks of historic early bookmakers.</p><br>
<p>The building was designed by Dwight and Chandler of Boston and completed in 1898. It was built as a gift to the town by Kingston native J. Howard Nichols, a Boston industrialist and philanthropist. The building is distinctive statewide as the only local library building exhibiting Shingle style and Richardsonian Romanesque features. The building served as a library until 2012, when the library relocated to new quarters at 2 Library Lane. The building now serves as a research library, specializing in genealogical research, and is an extension of the Kingston Community Library, housing the towns archives and the Kingston Historical Museums collections.</p><br>
<p>The Old North Hampton Library is a historic library building at 237 Atlantic Avenue in North Hampton, New Hampshire. The small, single-story Tudor Revival structure was designed by Boston architect J. Lawrence Berry and built in 1907. It was the town&#39;s first purpose-built library building, and was used as such until a new library was built nearby in 1973. It presently houses town offices. The building was listed on the National Register of Historic Places in 2014.</p><br>
<h2>Description and history</h2><br>
<p>The former North Hampton Library building is located in a cluster of municipal buildings on the north side of Atlantic Avenue (New Hampshire Route 111), a short way east of its junction with Lafayette Road (United States Route 1). It is a single-story structure, with fieldstone end walls and a side gable roof. The front facade is fieldstone (a continuation of the foundation) up to the bottoms of the windows, and is then finished in a half-timbered effect above. The main entrance is at its center, sheltered by projecting gabled portico with large timber brackets. It is flanked on the roof face by two eyebrow dormers. An addition, built in 1955, extends to the buildings rear. The towns modern library is set further back on the same lot.</p><br>
<p>North Hamptons public library was established in 1892, after the state passed enabling legislation encouraging the creation of such public facilities. It was originally housed in town hall, and a drive to build a dedicated facility began in 1899. Boston architect J. Lawrence Berrys first design, submitted in 1904, was rejected by the town meeting as too expensive to build, and the present design was accepted and built in 1907. The new library was built in 1973, and this building has since housed town offices.</p><br>
<p>The Hogan Group is a collection of six  islands and islets located in the Bass Strait that define part of the border between mainland Australia and the island state of Tasmania. Within the jurisdiction of Tasmania, the Hogan Group forms a land border between the states of Tasmania and Victoria. The island group is officially designated unallocated Crown land, within the Flinders Municipality in Tasmania and the South Gippsland Shire in Victoria.</p><br>
<p>The Hogan Group comprises the Hogan Island, Twin, Long, Round, East, Boundary (or North East) islets, and Seal Rock.</p><br>
<h2>Location and geography</h2><br>
<p>The Hogan Group is located 40 km southeast of Wilsons Promontory in the Bass Strait. The islands are made up of grey and red granite and limestone. A group of fur seals live on Boundary Islet. Other plants and animals that live on and near the island group include Cystophora intermedia, eelgrass, kelp, and abalone.</p><br>
<h2>History</h2><br>
<p>During the Pleistocene period, The Hogan group was part of a land bridge that connected Tasmania to mainland Australia. After the glacial period ended, the Hogan Group were the first group of islands to become isolated by rising sea levels.</p><br>
<p>The Hogan Group was discovered by Europeans and named in 1801 by John Black, captain of the Harbinger who named the island group after Michael Hogan, the owner of his ship. There are records of settlers on the island group, who hunted seals and kangaroos and used the islands for grazing land. On 12 October 1900, the first lease was recorded and given for Hogan Island. While the original lease covered the entire island group, since 1959 the lease has only applied to Hogan Island, which has been leased by B.R. Stackhouse since 1967, who uses the island for sheep and cattle grazing.</p><br>
<p>Black erred in his initial survey, placing the group further north than they actually are, which led to the Victoria-Tasmania land border on Boundary Islet.</p><br>
<p>St. Frances Cabrini Catholic Church is a historic Catholic church building in Omaha, Nebraska, United States. It was formerly the cathedral of the Diocese of Omaha and was named St. Philomena&#39;s Cathedral at that time. The church and the rectory are listed on the National Register of Historic Places and are also Omaha Landmarks under the St. Philomena name.</p><br>
<h2>History</h2><br>
<p>The Spanish Renaissance Revival style church was built in 1908 as St. Philomenas Cathedral. It served the Diocese of Omaha as its cathedral church until St. Cecilias Cathedral was substantially completed in 1916. The church was designed by Omaha architect Thomas Rogers Kimball. The name of the church was changed in 1958 to honor the first American citizen to be canonized a saint, Frances Xavier Cabrini. It was named an Omaha Landmark in 1979 and it was added to the National Register in 1980.</p><br>
<p>The Col de Val Louron-Azet   is a mountain pass in the French Pyrenees in the department of Hautes Pyrenees, which links Saint-Lary-Soulan and Azet, in the Aure Valley to the west, with Génos and Loudenvielle in the Louron Valley to the east. To the east of the pass is the Val-Louron ski station, and the GR10 footpath is also nearby.</p><br>
<h2>Details of climb</h2><br>
<p>Starting from Génos, the hairpin climb is 7.4 km long. Over this distance, the climb is 622 m at an average gradient of 8.3%, with the steepest section being at 13%.</p><br>
<p>Starting from Bazus-Aure, near to Saint-Lary-Soulan, the climb is 12 km long. Over this distance, the climb is 807 m at an average gradient of 6.7%, with the steepest sections being at 11.8%.</p><br>
<h2>Appearances in Tour de France</h2><br>
<p>The Col de Val Louron-Azet was first used in the Tour de France in 1997, since when it has featured six times, most recently in 2014.</p><br>
<p>The Galesburg Historic District is a 496 acre historic district in Galesburg, Illinois. The district includes 1049 contributing buildings and contains the towns original plat as well as several older neighborhoods. The section of the district south of North Street encompasses Galesburgs historic city center and its most significant landmarks, such as the Knox County Courthouse, the Knox County Jail, the Burlington Depot, and Main Street&#39;s commercial buildings. Knox College, the school Galesburg was founded to serve, and its historic Old Main are also located in the southern half of the district. The area north of North Street is mainly residential and is dominated by Queen Anne and Classical Revival houses, including many transitional houses displaying elements of both styles.</p><br>
<p>The district was added to the National Register of Historic Places on November 21, 1976.</p><br>
<p>The North Hampton Town Hall is located at 231 Atlantic Avenue in North Hampton, New Hampshire. Built in 1844, it was the town&#39;s first purpose-built municipal building, and continues to be used as such. Its construction includes materials recovered from older dual-purpose religious and civic buildings, and its tower houses a Revere bell. The building was listed on the National Register of Historic Places in 2013.</p><br>
<h2>Description and history</h2><br>
<p>The North Hampton Town Hall stands amid a cluster of civic buildings on the north side of Atlantic Avenue (New Hampshire Route 111), a short way east of its junction with Lafayette Road (United States Route 1. It is a single-story white clapboarded building with a two-stage tower, in which hangs an 1816 Revere bell. The tower&#39;s pyramidal roof and clock were added in 1920. The building corners have Greek Revival pilasters, which rise to an entablature and a fully pedimented gable. At the center of the gable is a half-oval fanlight in the Federal style. There is a single main entrance, placed at the center of the front facade, with sash windows on either side. Both the windows and entrance are trimmed by narrower Federal-style moulding.</p><br>
<p>The structure was built in 1844 to serve the towns municipal needs, a function it continues to serve today. It was built about one-quarter mile east of the previous meetinghouse, which served both civic and religious functions, and marked a shift in the civic center of the community to a point nearer the railroad, which passes north-south just east of the municipal complex. In addition to the bell, which originally hung in the towns second meetinghouse, the building includes timbers from meetinghouses built 1734 and 1761.</p><br>
<p>The North School, also known locally as the Brick School, is a historic one-room schoolhouse at 63 Amesbury Street in Kensington, New Hampshire, United States. Built in 1842, it was the only brick schoolhouse built in the town, and is one of its four surviving 19th-century schools. Of those, it is the best-preserved, and is used as a local history museum. It served the town&#39;s educational purposes between 1842 and 1956, and is now a local history museum. The building was listed on the National Register of Historic Places in 2013.</p><br>
<h2>Description and history</h2><br>
<p>The North School is located north of the small village center of Kensington, in a rural setting at the northwest corner of Amesbury Street (New Hampshire Route 150) and Moulton Ridge Road. It is a single-story gable-roofed brick building, with a small wood-frame addition to one side. Oriented facing south, its front facade is one of the gable ends, with three window bays to the left of the building entry. Windows are rectangular sash, and are set in openings that lack adornment; the entry door is topped by a four-light transom window, and there is a smaller sash window in the gable. The building interior includes a small vestibule area and a large classroom space, with outhouse facilities in the otherwise unfinished frame addition. The interior is finished with late 19th and early 20th-century finishes.</p><br>
<p>The school was built in 1842 on the site of a previous school dating to 1798. It has seen primarily modest alterations since its construction, most notably the addition of windows on its west side in 1918, the installation of the ell for toilet facilities in 1920, and the provisioning of electricity in 1938. It is maintained by the Kensington Historical Society, which was formed in 1971 to preserve it.</p><br>
<p>The Union Meetinghouse or Universalist Church is a historic church building at 97 Amesbury Road in Kensington, New Hampshire. Built in 1839-40, it is a well-preserved and little-altered example of a mid-19th century Greek Revival rural church. It was listed on the National Register of Historic Places in 2013, and continues to be used for summer services.</p><br>
<h2>Description and history</h2><br>
<p>The Union Meetinghouse stands at the southern end of a cluster of civic and municipal buildings that constitute the town center of Kensington, at the junction of Amesbury and Osgood Roads. It is a single-story wood frame structure, with a gabled roof and clapboarded exterior. Its main facade has a pedimented gable and a pair of doorways, each flanked by sidelight windows and topped by an entablature. The church tower has two stages, and is topped by Gothic pinnacles at the corners (a later addition). The building has seen only relatively minor alterations since its construction. The interior retains its original as-built configuration, with original pulpit and fixtures.</p><br>
<p>The single story Greek Revival white clapboard structure was largely completed in 1839 and formally dedicated in 1840. It was originally built to serve as a meetinghouse shared by several Protestant congregations, partly the result of splits within the dominant Congregationalists, and partly due to the rising number of Baptists and Quakers in the community. By 1865 many of these congregations had either folded or established their own buildings, leaving the building to the large Universalist congregation. The town formally deeded the underlying land to the Universalist Society in 1915.</p><br>
<p>McCord House, also known as the McCord-Oxner House, is a historic home located at Columbia, South Carolina. It built in 1849, and is a 1 1/2-story clapboard Greek Revival style cottage, with additions made in the 1850s. It sits on a stuccoed raised basement. The front facade features a one-story portico supported by four stuccoed piers. It was built by David James McCord , planter, lawyer and editor, and his wife Louisa Susannah Cheves McCord, a noted author of political and economic essays, poetry and drama. In 1865, the McCord House became the headquarters of General Oliver O. Howard, who was General William Tecumseh Sherman’s second in command.</p><br>
<p>It was added to the National Register of Historic Places in 1979. The house is currently owned by Henry McMaster, the incumbent Governor of South Carolina, who purchased the property in May 2016.</p><br>
<p>Taylor House, also known as the former home of the Columbia Museum of Art, is a historic home located at Columbia, South Carolina. It designed by the noted architectural firm of Andrews, Jacques and Rantoul and built in 1908, as a two-story, "L"-shaped, brick Neo-Classical style mansion. The front facade features a projecting portico supported by large, fluted limestone Corinthian order columns. It was built for Thomas Taylor, Jr., who served as president of Taylor Manufacturing Company. In 1950, the Columbia Museum of Art converted the house for use as a museum. The museum added three wings. The original stables are joined to the main house by the Science Museum wing.</p><br>
<p>It was added to the National Register of Historic Places in 1982.</p><br>
<p>The Doyle-Benton House was the former residence of James and Daphne Doyle until 1904, where it was later the residence of Frank Benton and family in 1906 until 1970. Mr. Doyle was the founder of the Portland Gold Mine, which is still producing as part of AngloGold Ashanti’s Cripple Creek and Victor Mining Company on the western slope of Pike’s Peak. Mr. Benton was a prominent cattle rancher on the Western Slope and was one of the founders of the National Western Stock Show.</p><br>
<h2>History</h2><br>
<p>Mr.Doyle was a flamboyant character whose business and personal situations were profiled in great detail in Denver newspapers during the late 1890s and early 1900s. Notwithstanding his troubles, he was clearly a likable individual as evidenced by his reelection as the mayor of Victor, Colorado while he was serving jail time for contempt of court in a business dispute with his partner. Doyle eventually lost both his wife and his fortune in the course of his protracted business litigation and ended up selling the house in 1904 to a dentist named George Schumacker. Schumacker only resided at the Doyle-Benton house for a short period of time- under two years- and then sold the house in 1906 to the Frank Benton family.</p><br>
<p>The Bentons owned the home for an ensuing 64 years until 1970. The Bentons were prominent cattle ranchers on the Western Slope and Frank was one of the founders of the National Western Stock Show. He was a prolific columnist and writer and authored a book called “Cowboy Life on the Sidetrack”, which depicted the difficulties ranchers had in sending their livestock via the Union Pacific railroad to slaughterhouses in the Midwest.</p><br>
<h2>Restoration</h2><br>
<p>The home had undergone major modifications sometime during the 1970s, and was converted into four separate apartments with exterior entrances for each room, complete with kitchens. In 2004, restoration efforts were contracted to The Cygnet Group to remove the modifications and restore the structure back to its original appearance with some modern upgrades, while keeping to the original appearance wherever possible.</p><br>
<p>Seal Island is an island located in Investigator Strait off the south coast of Yorke Peninsula in the Australian state of South Australia about 7 km south south-west of Stenhouse Bay. Since 1972, it has been part of the Althorpe Islands Conservation Park.</p><br>
<h2>Description</h2><br>
<p>Seal Island is about 7 km south south-west of Stenhouse Bay. It is described as an ‘elevated hump’ rising to a height of 35 m with a series of ‘segmented islets’ at its west side. Seal Island is reported as being best accessed via its north coast and during the ‘calmest weather’.</p><br>
<p>A number of sources consider Seal Island along with the Althorpe Islands and Haystack Island to be a group of islands known as the Althorpe Islands Group.</p><br>
<h2>Formation, geology and oceanography</h2><br>
<p>Seal Island was formed between 7500 and 8900 years ago after sea levels rose at the start of the Holocene thereby separating Yorke Peninsula from Kangaroo Island.</p><br>
<p>Seal Island is the remains of a granite inselberg capped by a layer of Bridgewater Formation calcarenite which has been extensively eroded by the action of the sea.</p><br>
<p>Seal Island rises from a depth of 20 m within 300 m to its west and south shores, and within 700 m of its east shore.</p><br>
<h2>Flora and fauna</h2><br>
<h3>Flora</h3><br>
<p>A survey carried out in 1996 reported that 10 species of plants to be present including Nitre-bush, Grey Samphire, Roundleaved Pigface, Sea Celery, Marsh Saltbush and Ruby Saltbush and Australian Hollyhocks.</p><br>
<h3>Fauna</h3><br>
<p>A survey carried out in 1996 reported the following vertebrate animals to be present - Black-faced cormorant, Little penguin, Sooty oystercatcher, Rock parrot, Silver gull and Fairy tern. The 1996 survey also noted the presence of Galahs and Australian sea lions but assumed these animals were not residents of the island.</p><br>
<h2>Protected areas status</h2><br>
<p>Since 1972, the island has been part of the Althorpe Islands Conservation Park. Since 2007, it has been a prohibited area where access is only allowed by permit in order to protect breeding population of seabirds. Since 2012, the waters surrounding its shores are part of a sanctuary zone located within the boundaries of the Southern Spencer Gulf Marine Park.</p><br>
<p>The Elsah Historic District is a 350 acre historic district in Elsah, Illinois. The district includes 48 contributing buildings which reflect the villages period of growth in the 1850s. Elsah was founded in 1853 as a riverfront town on the Mississippi River; by 1861, it had grown to its current size, as geographic and economic limitations prevented further expansion. The towns 1861 appearance is well-preserved, and three distinct areas of the town have gone almost entirely unchanged since. The historic commercial district on LaSalle Street, which extends three blocks inward from the river, consists mainly of stone buildings; all but one of its pre-1861 buildings, including all four of the village&#39;s historic taverns, still stand. The other two districts are both located on Mill Street and are primarily residential; the larger one is three blocks long and has an assortment of stone and brick houses, while the smaller section has a single block of Greek Revival homes.</p><br>
<p>The district was added to the National Register of Historic Places on July 27, 1973.</p><br>
