NoeFlandre/osm-polygon-wikidata-only huggingface dataset:
Clear Lake (Douglas County, Oregon)

Clear Lake is a natural body of water impounded by sand dunes along the Oregon Coast of the Pacific Ocean in the United States. The lake is the municipal water supply for the city of Reedsport, which lies about 4 miles (6 km) northeast of the lake. Clear Lake is closed to public access to protect the purity of the water. U.S. Route 101 runs north–south along the west side of the lake. The community of Winchester Bay is north of the lake; Umpqua Lighthouse State Park and the mouth of the Umpqua River are to the northwest, and Oregon Dunes National Recreation Area runs along the coast to the west. The outflow from Clear Lake is south to Edna Lake, Clear Creek, and Eel Lake. Clear Lake, at 229 feet (70 m) above sea level, is the highest of several lakes formed by dunes encroaching on Clear Creek's ancestral valley. Water from this string of lakes, including Eel Lake and Tenmile Lake, flows generally south into Tenmile Creek in Coos County, which flows west into the Pacific near the community of Lakeside. See also List of lakes in Oregon References External links Annual Water-Quality Reports for Reedsport
Clear Lake (Linn County, Oregon)

Clear Lake is a mountain lake 86 mi (138 km) northeast of Eugene, Oregon, United States in Linn County. It has two main bodies connected by a bottleneck. The lake is primarily fed by snow runoff from nearby Mount Washington and the surrounding areas. The runoff filters through caverns for more than 20 years before emptying into Clear Lake. The lake is also fed by two small creeks, which may dry up seasonally, along with Great Spring, the source of the McKenzie River. Clear Lake is the headwaters of the McKenzie River, which is the sole source of drinking water for Eugene. The south end of Clear Lake empties 250,000 gallons per minute (57 million Liters/hour) into the White Water Rapids which then flows over Sahalie Falls and Koosah Falls 1 mile downstream on the opposite side of Highway 126. Diving Clear Lake is reported to be one of the most exceptional freshwater dive spots in Oregon. Submerged 100 feet (30 m) deep in the lake is a stand of upright trees that were killed approximately 3,000 years ago when volcanic activity created the lake. The trees are remarkably preserved due to the cold year-round water temperatures of between 35–43 °F (2–6 °C). Hiking Clear Lake is circled by Clear Lake Loop Trail, a hike loop made up of Clear Lake Trail and McKenzie River Trail that is 5 miles (8.0 km) long. An accompanying trail guide prepared by Willamette National Forest tells visitors about Clear Lake and the neighboring lava field and forest. See also List of lakes in Oregon References External links Media related to Clear Lake (Linn County, Oregon) at Wikimedia Commons "Clear Lake". Geographic Names Information System. United States Geological Survey, United States Department of the Interior.
Lac Clear (Oregon)

Le lac Clear est un lac de montagne situé à 138 km d'Eugene, dans l'État de l'Oregon aux États-Unis. Il est composé de deux bassins principaux reliés par un goulot d'étranglement. Le lac est principalement alimenté par les eaux de ruissellement de la neige à proximité du Mont Washington et les zones environnantes. Les eaux s'infiltrent et ruissellent à travers des cavernes souterraines pendant plus de 20 ans avant de se jeter dans le lac. Le lac est également alimenté par deux petits ruisseaux qui peuvent se tarir suivant la saison. Le lac Clear devient la rivière McKenzie qui est la source d'eau potable de la ville d'Eugene. Plongée Le lac est réputé pour la clarté de ses eaux qui permettent la pratique de la plongée. Les plongeurs peuvent observer, à 30 m de profondeur, un ensemble d'arbres qui ont été immergés depuis près de 3 000 ans, lorsque l'activité volcanique a créé le lac. Les arbres sont remarquablement conservés en raison des températures froides de l'eau toute l'année comprises entre 1,6 à 6 °C. Images Source (en) Cet article est partiellement ou en totalité issu de l’article de Wikipédia en anglais intitulé « Clear Lake (Linn County, Oregon) » (voir la liste des auteurs). Liens externes Ressource relative à la géographie : Geographic Names Information System Portail de l’Oregon Portail des lacs et cours d'eau
Клир-Лейк (озеро, округ Линн, Орегон)

Клир-Лейк (англ. Clear Lake) — горное озеро в 138 километрах к северо-востоку от города Юджин, штат Орегон, США, в округе Линн. Оно состоит из двух основных частей, соединённых между собой узким проливом. История Озеро питается преимущественно снеговыми водами с близлежащей горы Вашингтон и прилегающих территорий. Вода проходит через систему пещер, где происходит её фильтрация, в течение более чем 20 лет, прежде чем попасть в Клир-Дейк. Также озеро получает воду из двух небольших ручьёв, которые могут пересыхать в зависимости от сезона, а также из источника Грейт-Спринг, который является истоком реки Мак-Кензи. Клир-Лейк является истоком реки Мак-Кензи, которая является единственным источником пресной воды для города Юджин. Южный конец озера Клир-Лейк сбрасывает 57 миллионов литров в час в пороги White Water, которые затем текут через водопады Sahalie Falls и Koosah Falls в миле ниже по течению на противоположной стороне шоссе 126. Отдых Сообщается, что Клир-Лейк является одним из самых уникальных мест для дайвинга в пресных водах штата Орегон. На глубине 30 метров в озере находятся вертикальные деревья, которые погибли около 3000 лет назад в результате вулканической активности, создавшей озеро. Деревья прекрасно сохранились благодаря круглогодичной температуре воды, которая колеблется от 2 до 6 градусов Цельсия. Озеро окружено пешеходным маршрутом Clear Lake Loop Trail, который состоит из двух участков: Clear Lake Trail и McKenzie River Trail. Общая протяжённость маршрута составляет 8 километров. Путеводитель по маршруту, подготовленный Willamette National Forest, содержит информацию о Clear Lake, соседнем лавовом поле и лесе. Примечания
Клір-Лейк (округ Линн, Орегон)

Клір-Лейк (з анг. "чисте озеро") — гірське озеро 138 км на північний схід від Юджина, штат Орегон (США) в окрузі Линн. Він має два основні корпуси, з’єднані вузьким горлечком. Озеро в основному живиться сніговим стоком із сусідньої гори Вашингтон та прилеглих територій. Стік фільтрується через печери більше 20 років, перш ніж впасти в Чисте озеро. Озеро також живиться двома маленькими струмками, які можуть пересихати сезонно, разом із Великим джерелом, джерелом річки Маккензі. Озеро Клір-Лейк є витоком річки Макензі, яка є єдиним джерелом питної води для Юджина. Дайвінг Повідомляється, що Клір-Лейк є одним з виняткових місць для дайвінгу в прісній воді в Орегоні. На глибині 30 м в озері спостерігаються прямостоячі дерева, які загинули приблизно 3000 років тому, коли вулканічна діяльність сформувала озеро. Дерева чудово збереглися завдяки холодній цілорічній температурі води 35–43 °F (1,6–6 °C). Піші прогулянки Озеро Клір-Лейк оточене стежкою Клір-Лейк-Луп, пішохідною петлею, що складається з Стежки Клір-Лейк-Трейл і Стежки Маккензі-Рівер, протяжністю 8 км. Супровідний маршрутний путівник, підготовлений Національним лісом Вілламетт, розповідає відвідувачам про Клір-Лейк і сусіднє лавове поле та ліс. Дивись також Список літератури Зовнішні посилання Вікісховище має мультимедійні дані за темою: Клір-Лейк (округ Линн, Орегон)
Clear Lake (Wasco County, Oregon)

Clear Lake is a mountain lake 53 miles (85 km) southeast of Portland, Oregon, United States in Mount Hood National Forest. It can be seen from flights in the region as a bird-shaped body of water. It is 12 miles (19 km) south of Mount Hood and 5 miles (8.0 km) northeast of Timothy Lake, near the junction of U.S. Route 26 and Skyline Road at the latter's northern terminus. It is near the northwest corner of Wasco County. The Pacific Crest Trail is 4 km (2 mi) west of the lake. It is fed by several small streams of the eastern Cascade crest. It is the headwaters of Clear Creek, a tributary of the White River, blocked at the east end by the Wasco Dam. The earthen dam was a 1959 irrigation project of the United States Bureau of Reclamation, 59 feet high and 1901 feet long at its crest. Clear Lake Butte is a 4,454 feet (1,358 m) butte 1.3 miles (2.1 km) south of the lake, and defines the northwest corner of Warm Springs Indian Reservation. The lake is known for abundant fish and its windy conditions. The banks are edged by tree stumps and free range cattle tracks. The campground has 28 established spots and an overflow area. See also Clear Lake (Oregon), for other lakes with the name List of lakes in Oregon References
Cleawox Lake

Cleawox Lake (klē' ə woks), is a body of water dammed by sand dunes along the Pacific Ocean coast of the U.S. state of Oregon. The lake is about 3 miles (5 km) south of Florence along U.S. Route 101. Sharing the lakeshore are private properties as well as Oregon Dunes National Recreation Area and Jessie M. Honeyman Memorial State Park, which also partly fronts on Woahink Lake. Cleawox is derived from the Siuslaw name for the lake. Geology Cleawox Lake is a submerged remnant of the headwaters of a small coastal stream that existed before the most recent ice age. The lake formed after melting glaciers caused a rise in sea level that drowned the lower reaches of the stream. Sediments from the sluggish stream formed sand dunes, behind which the lake was dammed. The dunes, estimated to be advancing northward at 15 to 20 feet (4.6 to 6.1 m) a year, are encroaching on the lake. Watershed Covering only 1.6 square miles (4.1 km2), Cleawox Lake's drainage basin is separate from the nearby Woahink–Siltcoos watershed to the east and south. Water enters Cleawox from small surface streams and by seepage, and no surface outflow has been identified. Soils are sandy and well-drained and support mainly pines and shrubs. Although the lake is saltier than most other coastal lakes in Oregon, it is also more transparent. About 2 miles (3 km) of the lakeshore borders Oregon Dunes National Recreation Area, and about 1 mile (1.6 km) borders Honeyman State Park. The rest borders private property, including vacation homes and girl scout Camp Cleawox. Recreation Park visitors use the lake for swimming, canoeing, and fishing for warm-water species and rainbow and coastal cutthroat trout. In the state park, picnic tables have been set up in sight of the water. No overnight camping is allowed next to the lake, but nearby areas of the state park have many campsites. See also List of lakes in Oregon References External links Media related to Cleawox Lake at Wikimedia Commons
Lac Cleawox

Le lac Cleawox (en anglais : Cleawox Lake) est un lac américain dans le comté de Lane, en Oregon. Il est situé à 24 mètres d'altitude derrière un cordon dunaire qui le sépare de l'océan Pacifique. Liens externes Ressource relative à la géographie : Geographic Names Information System Portail des lacs et cours d'eau Portail de l’Oregon
Клиуокс

Клиуокс (англ. Cleawox) — бессточное солоноватое озеро на побережье Тихого океана в округе Лейн, Орегон, США. Находится примерно в 3 км южнее Флоренса. Площадь поверхности озера оценивается в 0,32 км², 0,33 км². Высота над уровнем моря составляет 24 или 23 м. Глубина оценивалась в 15 м в 1954 году, однако с тех пор наблюдается заполнение озёрной котловины песчаными отложениями. В 2008 году зафикисирована глубина 12 м. Объём воды в 1954 году составлял 1,716 млн м³ (1391 акр-фут). Протяжённость береговой линии — 8 км. Озеро образовалось в результате затопления верховьев небольшого прибрежного ручья во время постледникового подъема уровня моря и последующего окаймления его берегов песчаными дюнами. По оценкам, дюны на его западном берегу продвигаются на север со скоростью примерно 5—6 м (15—20 футов) в год. Озеро имеет приток Бак-Крик. С 1939 года дюны южного берега Клиуокса сместились примерно на 150 метров на север со средней скоростью 2,3 метра в год. Несмотря на низкую популярность рыбалки в озере, Клиуокс активно используется в качестве места для купания, гребли на каноэ и пикников. Рядом с водоёмом располагается лагерь для девочек-скаутов. На берегах озера — Национальная зона отдыха Дюны Орегона (около 3 км береговой линии) и Государственный парк Ханимен (1,6 км). Название озера происходит из языка саюсло, где звучало как klē' ə woks. Примечания
Universidad de Portland

La Universidad de Portland (University of Portland en idioma inglés), es una universidad privada, católica, de la Congregación de Santa Cruz, ubicada en la ciudad de Portland, Oregón (Estados Unidos de América). Historia En un viaje en barco por el río Willamette, Alexander Christie, Arzobispo de Portland, se fijó en un edificio que divisó en una ladera y averiguó que se trataba de "West Hall", un edificio abandonado que había sido sede de una universidad de la Iglesia Metodista Episcopal fundada en 1891 y cerrada en 1900. La arquidiócesis de Portland y la Congregación de Santa Cruz decidieron adquirir el edificio y sus terrenos y abrieron las puertas de la actual Universidad de Portland el 5 de septiembre de 1901 a la primera promoción de 52 alumnos. Sus 8 profesores eran todos sacerdotes católicos. En 1902´, la propiedad pasó a ser en su totalidad de la Congregación de Santa Cruz. Centros docentes Consta de cinco facultades y escuelas: College of Arts & Sciences Pamplin School of Business School of Education School of Engineering School of Nursing Deportes Portland compite en la West Coast Conference de la División I de la NCAA. Referencias Enlaces externos Web oficial
Université de Portland

L'université de Portland (en anglais : University of Portland) est une université catholique privée américaine située à Portland dans l'État de l'Oregon aux États-Unis. Elle est affiliée à la congrégation de Sainte-Croix et jumelée à l'université Notre-Dame. Fondé en 1901, l'établissement compte à l'automne 2019 environ 4 200 étudiants. Histoire Personnalités liées à l'université Professeurs Étudiants Liens externes (en) Site officiel Portail des universités américaines Portail du catholicisme Portail de Portland
Università di Portland

L'Università di Portland (University of Portland, citata anche con la sigla UP) è un'università cattolica statunitense con sede a Portland, Oregon, affiliata alla Congregazione di Santa Croce, che ha fondato anche la consorella Università di Notre Dame. Fondata nel 1901, la UP ha un corpo studentesco di circa 4 000 allievi e, per il 2018, è classificata al sesto posto tra le università regionali occidentali secondo U.S. News & World Report. Il campus è situato allo University Park vicino al quartiere St. Johns, su un promontorio che domina il fiume Willamette. Grazie alla presenza di collegio di arti e scienze, una scuola di specializzazione, e scuole di commercio, istruzione, ingegneria e infermieristica, è l'unica università cattolica completa nello stato dell'Oregon. È la più grande corporation nell'area di North Portland, creando un indotto di circa $ 170 milioni annuale sulle attività economiche di Portland. Più di 13 000 alunni vivono nell'area metropolitana di Portland. Sport Le squadre della sezione di atletica, presenti in diverse discipline sportive tra cui calcio, maschile e femminile, pallavolo e pallacanestro, sono denominate Portland Pilots e competono nella Division I della National Collegiate Athletic Association (NCAA). Note Altri progetti Wikimedia Commons contiene immagini o altri file su University of Portland Collegamenti esterni (EN) Sito ufficiale, su up.edu. University of Portland (canale), su YouTube. (EN) Università di Portland, in Catholic Encyclopedia, Robert Appleton Company.
Универзитет у Портланду

Универзитет у Портланду (енгл. University of Portland) је приватни католички универзитет у Портланду. Основан је 1901. године и повезан је са Конгрегацијом Светог крста, која је такође основала Универзитет Нотр Дам. На Универзитету у Портланду студира око 3.730 студената. Галерија Референце Спољашње везе Званични веб-сајт
Coalman Glacier

The Coalman Glacier (also Coleman Glacier) is a glacier located on the upper slopes of Mount Hood in the U.S. state of Oregon. It is the mountain's highest glacier ranging from about 11,200 to 10,500 ft (3,400 to 3,200 m), located within the crater rim, southwest of the peak. It was named for Elija Coalman (variously spelled Elijah Coleman), an early mountain guide who climbed Mount Hood 586 times. Coalman Glacier is the second most frequently visited glacier on the mountain because it is part of the popular South Climbing route from Timberline Lodge. It lies entirely within Mount Hood Wilderness. The most well known feature of Coalman is the Hogsback: a snow ridge running southwest to northeast from Crater Rock toward the summit ridge. The Bergschrund is another widely known feature where the glacier pulls away from the stagnant ice leaving a large crevasse. In 2007, it had become large enough to cause most climbers to use another route. The glacier is a remnant of the massive glaciers that formed during the last ice age. It is historically known to change configuration dramatically, at times a gradual, smooth surface to Hot Rocks; at other times the same place has a 40 ft (12 m) ice cliff. The glacier flows southwest, and is bounded on the north and east by the summit, on the northwest by the rocky crater wall known as Castle Crags (also Hawkins Cliffs), on the west by Hot Rocks, and on southeast by the back side of Steel Cliff. Climate Hawkins Ridge lies on the upper western edge of Coalman Glacier. There is no weather station, but this climate table contains interpolated data. See also List of glaciers in the United States References
Coast Guard Air Station North Bend

Coast Guard Air Station North Bend (CGAS North Bend) was established September 28, 1974 at Southwest Oregon Regional Airport in North Bend, Oregon, United States. The unit houses 153 active duty, nine reserve duty and five civilian personnel. The unit operates five Eurocopter HH-65 Dolphin helicopters. CGAS North Bend received its first upgraded HH-65C Dolphin in 2007 The unit functions include search and rescue, law enforcement, marine environmental protection, aids to navigation, and enforcement of federal treaties. References External links CGAS North Bend website
Coburg Historic District

The Coburg Historic District is a National Historic District located in the city of Coburg, Oregon, United States. The district is roughly bounded by Van Duyn Road, Diamond and Miller streets, Dixon Street and Tax lots 1700 and 201, and Bottom Loop Road. The district was placed on the National Register of Historic Places in 1986. The period of significance of the district dates back to 1875. References External links Media related to Coburg Historic District at Wikimedia Commons Information on historic homes from the City of Coburg website
Ashland Downtown Historic District

The Ashland Downtown Historic District in Ashland, Oregon is a 32.2 acres (13.0 ha) historic district (United States) which was listed on the National Register of Historic Places in 2000. The district is roughly bounded by Lithia Way and C Street, Church, Lithia Park and Hargadine and Gresham Streets. The listing included 55 contributing buildings and six contributing objects, as well as 26 non-contributing buildings and one non-contributing object. Eleven buildings were already separately listed on the National Register. Buildings include: Ashland Masonic Lodge Building, NRHP-listed in 1992 Ashland IOOF Building, or IOOF Building NRHP-listed in 1978 Citizen's Banking & Trust Co. Building, 232-242 E. Main St., NRHP-listed in 1985 Enders Building, 250–300 E. Main St., NRHP-listed in 1986 First Baptist Church (1911), 241 Hargadine Street, NRHP-listed in 1979 First National Bank, NRHP-listed in 1980 Ashland Springs Hotel, also known as the Lithia Springs Hotel and as the Mark Antony Motor Lodge, NRHP-listed in 1978 Fordyce & Julia Roper House, NRHP-listed in 1985 Trinity Episcopal Church, NRHP-listed in 1984 Vaupel Store and Oregon Hotel Building, NRHP-listed in 1980 Whittle Garage Building, NRHP-listed in 1997, and Ashland's City Hall. Contributing objects include: Carter Memorial Fountain See also National Register of Historic Places listings in Jackson County, Oregon References External links Media related to Ashland Downtown Historic District at Wikimedia Commons
Collier Glacier

Collier Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range at an elevation generally above 8,000 feet (2,400 m). Collier Glacier is on the west slopes of North Sister, an extinct shield volcano. Since its last maximum extent during the Little Ice Age (1350–1850 A.D.) the glacier has retreated over a mile. See also List of glaciers in the United States References External links Media related to Collier Glacier at Wikimedia Commons Information about Collier Glacier on glaciers.us
Glacier Collier

Le glacier Collier (en anglais : Collier Glacier) se trouve dans l'État de l'Oregon, aux États-Unis. Le glacier est situé dans la chaîne des Cascades, sur le flanc ouest du volcan North Sister à une altitude supérieure à 2 400 mètres. Notes et références Liens externes Ressource relative à la géographie : Geographic Names Information System Portail des lacs et cours d'eau Portail de la montagne Portail de l’Oregon
Кольєр (льодовик)

Льодовик Кольєр (англ. Collier Glacier) — гірський льодовик в окрузі Лейн, у штаті Орегон, США. Географія Льодовик лежить на схилах вулканів Три Сестри (північний схил стратовулкана Середня Сестра та західний схил щитового вулкана Північна Сестра) у Каскадному хребті на висоті, як правило, понад 2400 м. З моменту останнього максимального поширення під час Малого льодовикового періоду (1350—1850 роки нашої ери) льодовик відступив приблизно на 1600 м. Льодовик довжиною 1500 м, займає площу 0,65 км² і містить близько 20 мільйонів м³ льоду. Див. також Список льодовиків у США Примітки Посилання Інформація про Collier Glacier на glaciers.us
Collins Beach (Sauvie Island)

Collins Beach is a sandy beach on the Columbia River side of Sauvie Island in Oregon, United States, located north of Portland. Part of it is a clothing-optional area. The beach is one mile (1.6 km) long and begins about 0.25 miles (400 m) after Reeder Road becomes gravel. Hours are 4:00 a.m. to 10:00 p.m. every day. The beach has been popular for nude use since at least the 1970s. It is surrounded by a 12,000-acre (49 km2) fish and game reserve, except for a 10-acre (4.0 ha) parcel of privately owned land west of Reeder Road at the north boundary of Collins Beach. Nude beach users continue onto the non-nude North Unit Beach which is poorly delineated and ineffectively screened from view, which has led to a legal complaint by the property owners. Collins Beach is one of two official clothing-optional beaches in Oregon after Glass Bar Island's in Eugene, Oregon closed. The other is Rooster Rock State Park. It is administered by the Oregon Department of Fish and Wildlife in cooperation with the Columbia County Sheriff's Office. See also Nudity in Oregon References External links Beaches – Sauvie Island Community Association Collins Beach – Outdoor Project
Columbia Southern Hotel

The Columbia Southern Hotel, also known as the Shaniko Hotel, is a historic hotel, located in Shaniko, Oregon, United States. Built by the Columbia Southern Railway in 1900–1902 at the southern terminus of its line, the hotel was and remains the most imposing structure in Shaniko. It was the hub and focal point of the community during the heyday of the local wool industry in the early decades of the 20th century. In addition to lodging, it served as saloon, bank, stagecoach stop, dance hall, and general gathering place. The hotel was listed on the National Register of Historic Places in 1979. In 1982 it was additionally listed as a contributing resource in the National Register-listed Shaniko Historic District. Gallery See also National Register of Historic Places listings in Wasco County, Oregon References