NoeFlandre/osm-polygon-wikidata-only huggingface dataset:
Ópera de Seattle

Seattle Opera House Marion Oliver McCaw Hall es la sala sede de la compañía de la Ópera de Seattle dirigida por Speight Jenkins y del Pacific Northwest Ballet en el estado de Washington (Estados Unidos) Inaugurada en 2003 fue construida utilizando la estructura de la antigua sede de la entidad original de la Feria Mundial de 1962. La sala tiene capacidad para 2890 espectadores. La rodea la Kreielsheimer Promenade diseñada por Gustafson Guthrie Nichol y conecta el edificio con el Seattle Center Campus. Se llevan a cabo las representaciones de El anillo del nibelungo con asistencia de audiencia y elencos internacionales. Enlaces externos Sitio oficial Datos técnicos Crítica del NYTimes
Lotus (motor vessel)

Lotus is a motor yacht, launched in 1909 in Seattle, Washington. Lotus was employed as a pleasure vessel on Puget Sound, and in the waters of British Columbia and southeastern Alaska. Lotus was of a unique design and is now on the National Register of Historic Places. Design and construction Lotus was built in 1908-1909 at Seattle, Washington for Maurice McMicken (1860-1940), a lawyer and businessman. The vessel was launched in May 1909, and was at that time the largest privately owned motor yacht on the west coast of the United States. The yacht was designed by naval architects Lee and Brinton, and constructed by Joseph A. Sloane. The yacht had accommodations for a party of 10 as well as a crew of four. The yacht carried enough fuel to have a range of 1,500 miles (2,400 km). As originally built, the vessel was 85 feet (26 m) long, 12.5 feet (3.8 m) beam, and 4.2 feet (1.3 m) in depth of hold. Overall size was 133 gross and 88 registered tons. Only two crew were required according to the 1911 merchant vessel registry. As of 1911, the vessel was powered with a "Globe" gas-distillate (early diesel) engine that generated 80 indicated horsepower. The vessel's U.S. Registry number was US registry # 206231 and the signal letters were L.B.C.M Career McMicken owned Lotus until his death in 1940. He used the yacht to cruise the waters of Washington, British Columbia, and southeast Alaska. Shortage of fuel forced the yacht to be tied up throughout the Second World War. McMicken's heirs sold the yacht in 1947. The yacht was sold again in 1951 to a family which moored the yacht in Lake Union and lived on it as a full-time residence. In 1961 the yacht was sold again, to Maj. (later Col.) Curtis Gruye, an Air Force officer, and a jet pilot. Gruye restored the yacht and operated it as a floating hotel for a number of years. In 1977, Gruye sold the yacht to Gordon R. Newell, an author and maritime historian. Newell moved the yacht to a marina in Olympia, where the yacht remained. In 1981, Gruye bought the yacht back from Newell, and began an extensive restoration program, which by 1982 was able to return the yacht to an operable condition. Current status Lotus was listed on the National Register of Historic Places in 1987. It is now maintained by the Motor Vessel Lotus Foundation, a non-profit, all-volunteer organization, and is moored in the Historic Ships Wharf at the Center for Wooden Boats in Seattle, Washington. Notes References National Register of Historic Places, Inventory – Nomination Form, “Motor vessel 'Lotus'” (March 31, 1987) (accessed 06-16-11) Newell, Gordon R., ed., H.W. McCurdy Marine History of the Pacific Northwest, Superior Publishing Co., Seattle, WA (1966) U.S. Dept. of the Treasury, Bureau of Statistics, Annual List of Merchant Vessels of the United States (for year ending June 30, 1911) (accessed 06-16-11). External links MV Lotus.org
Canon (bar)

Canon is a cocktail bar in Seattle, Washington, United States. Located on 12th Avenue near Seattle University, the bar has been recognized for having the "World's Best Spirits Selection". Description Thrillist has described Canon as a "snug bespoke whiskey bar and bitters emporium" with the world's largest selection of American whiskey. Condé Nast Traveler has described Canon as "world-class cocktails in a glowy spirits library where pretty booze bottles twinkle and shine". In 2017, Aimee Rizzo of The Infatuation wrote, "Canon is the Willy Wonka's Chocolate Factory of cocktails. The encyclopedic menu has pages upon pages of classic mixed drinks and original ones with intricate involvements like smokes, syrups, rinses, and/or Cap'n Crunch-infused ice cream floating on top. Plus, everything is served in whimsical vessels like light bulbs, Russian nesting dolls, glass hearts you wear around your neck, or IV bags that drip into your glass. Once you decide which nuanced masterpiece in mixology to order, watch the bartenders gather the ingredients from the bookshelves of liquors so massive they need their own Dewey Decimal System." Drinks have included the Canon Cocktail (rye, Ramazzotti, triple sec foam, bitters) and the Campfire in Georgia (mezcal, peach-habanero shrub, orange juice, cinnamon French oak, bitters). The Mandalorian Milk has dark rum, cacao, spicy vanilla citrus, green chartreuse, hemp milk, and bitters. The DK Ain't Got Sh*t On Me is served in a Donkey Kong game cartridge and has Japanese whiskey, rosé aperitif, banana, and chapparel. The Mrs. Eale's Receipt is served in a cone with ginger smoke and has bourbon, dark rum, oloroso sherry, vanilla, and ceylon. History Jamie Boudreau is the owner. The business closed temporarily, during the COVID-19 pandemic. Reception Seattle Magazine named Canon the city's best new bar in 2012. Canon placed sixth in Drinks International's 2014 list of The World's 50 Best Bars. Chona Kasinger included the business in Thrillist's 2014 list of Seattle's ten best whiskey bars. The website's Naomi Tomky and Bradley Foster included Canon in a 2022 list of "The Absolute Best Bars in Seattle Right Now". The Infatuation's Aimee Rizzo included Canon in a 2023 list of Seattle's 19 best bars. References External links Official website
Parafia św. Małgorzaty Szkockiej w Seattle

Parafia św. Małgorzaty Szkockiej w Seattle (ang. St. Margaret of Scotland Parish) – parafia rzymskokatolicka położona w Seattle w stanie Washington w Stanach Zjednoczonych. Jest ona wieloetniczną parafią w archidiecezji Seattle, z mszą św. w j. polskim dla polskich imigrantów. Nadzór klerycki nad parafią ma Towarzystwo Chrystusowe dla Polonii Zagranicznej. Parafia została poświęcona św. Małgorzacie Szkockiej. Historia W 1910 roku, Ojcowie Redemptoryści założyli misję która obsługiwała parafię Najświętszego Serca przy Warren Avenue N., w pobliżu obecnego Seattle Center. Kościół ten został wybudowany wkrótce potem przy West 14th Avenue i West Bertona, a następnie, w 1914 roku, został przeniesiony na obecne miejsce. W 1923 roku, parafia założyła szkołę, która została zamknięta w 1971 roku. Na jej miejscu, w 1977 roku, w sąsiedztwie kościoła, powstał ogród, nazwany Corboy Park, na cześć długoletniego proboszcza tej parafii. Jednak początek stałej opieki duszpasterskiej dla Polonii datowany jest od 1983 roku. Duży napływ z Polski tak zwanej fali solidarnościowej spowodował, że ks. Mieczysław Szwej S.Ch. dojeżdżał w każdą niedzielę po południu do Seattle, z parafii Świętych Apostołów Piotra i Pawła w Tacoma. Pierwsza msza św. była celebrowana w Domu Polskim, a potem już na stałe w kościele Św. Brygidy. Jesienią 1988 roku, ks. Mieczysław Szwej S.Ch. został przeniesiony do Kanady, a jego miejsce zajął ks. Józef Calik S.Ch. Rozpoczęto zbierać funduszy na polski kościół. W sierpniu 1992 roku, Arcybiskup Seattle, Thomas Murphy, wysłuchał próśb Polaków o miejsce dla odprawiania mszy św. w j. polskim, i przydzielił im zaniedbany kościół św. Małgorzaty Szkockiej. 6 września 1992 roku, pierwszą Mszę św., w odremontowanym kościele, odprawił Przełożony Generalny Towarzystwa Chrystusowe dla Polonii Zagranicznej ks. Bogusław Nadolski S.Ch. z Poznania, w towarzystwie ks. Prowincjała Tadeusza Winnickiego i ks. Józefa Calika S.Ch., którego Arcybiskup Seattle mianował kapelanem dla Polaków z prawami proboszcza. 19 stycznia 2004 roku, po krótkiej chorobie, niespodziewanie umiera ks. Józef Calik S.Ch. Po śmierci wieloletniego proboszcza, przez kilka miesięcy, obowiązki proboszcza piastował ks. Stanisław Kuczaik S.Ch., a od października 2004, proboszczem został ks. Stanisław Michałek S.Ch. Kościół ten jest jednym z najmniejszych i najstarszych katolickich kościołów w Seattle. Za kościołem jest kamienne sanktuarium wzniesione przez imigrantów polskich i oddane w 1993 roku. Bibliografia The Official Catholic Directory in USA. (ang.). St. Margaret of Scotland Church – Historical Site, Seatttle.gov (ang.) Linki zewnętrzne Archidiecezja Seattle (ang.) St. Margaret of Scotland – The Diocesian Directory (ang.)
Lake Rasmussen

Lake Rasmussen is a small lake in Duvall, Washington, a city in King County. The lake is home to a small public park. It has suffered from infestation by invasive aquatic weeds. Description Lake Rasmussen has a small public park on its western shore. The park includes picnic tables and wildlife viewing opportunities. In 2021 an eight-year old discovered invasive Egeria densa in the lake. Egeria densa is a noxious aquatic weed that grows densely, depriving native species of habitat and oxygen. This weed had never been found in the local watershed before, and it is speculated to come from an aquarium that was dumped into the lake. Goldfish were also found, further confirming this hypothesis. King County noted that Egeria was not yet widespread in the watershed when it was discovered, so herbicides were used to control the weed. References
Borealis Glacier

Borealis Glacier is in North Cascades National Park in the U.S. state of Washington and is on the north slopes of Primus Peak. Borealis Glacier flows generally northeast for a distance of approximately .70 mi (1.13 km). Borealis Glacier descends from nearly 7,200 to 6,000 ft (2,200 to 1,800 m), but is split into an upper and lower sections. The upper section is as much as .90 mi (1.45 km) wide, but ends abruptly in an icefall along some cliffs. The lower section has been retreating significantly, and between 1990 and 2009 lost almost 250 m (820 ft) in length, creating a proglacial lake at the terminus. See also List of glaciers in the United States References
Boston-Gletscher

Der Boston-Gletscher liegt in einem großen Kar unterhalb mehrerer Berggipfel im North Cascades National Park im US-Bundesstaat Washington. Der Gletscher ist schätzungsweise 1 mi (1,6 km) lang aber fast 3,5 mi (5,6 km) breit und der größte im North Cascades National Park. Während er sich in einem Bogen vom Norden des Forbidden Peak aus ausdehnt, wird der Gletscher auch vom Boston Peak im Südwesten und vom Buckner Mountain an seiner Ostseite flankiert. Zwischen dem Boston Peak und dem Buckner Mountain liegt der Gletscher unterhalb eines als Ripsaw Ridge bekannten Grates. Ein weiterer Grat erstreckt sich zwischen Boston Mountain und Forbidden Peak und weiter nordwärts und trennt den Boston-Gletscher von den benachbarten Quien-Sabe- und Forbidden-Gletscher. Der Boston-Gletscher befand sich seit dem Ende der Kleinen Eiszeit um das Jahr 1850 auf einem allgemeinen Rückzug. Ein mäßiges Wachstum gab es zwischen 1950 und der Mitte der 1970er Jahre, doch zwischen 1972 und 2006 zog sich der Gletscher erneut um 1.470 ft (448 m) zurück. Einzelnachweise Weblinks Boston Glacier. In: Geographic Names Information System. United States Geological Survey, United States Department of the Interior, abgerufen am 26. Oktober 2014 (englisch).
Boston Glacier

Boston Glacier is located in a large cirque below several mountain peaks in North Cascades National Park in the U.S. state of Washington. Approximately 1 mi (1.6 km) long but nearly 3.5 mi (5.6 km) wide, it is the largest glacier in North Cascades National Park. Extending in an arc from the north of Forbidden Peak, it is flanked by Boston Peak to the southwest and Buckner Mountain at its eastern margin, between which it lies below the arête known as Ripsaw Ridge. Another arête extending between Boston Peak, Sharkfin Tower, Forbidden Peak and further north separate Boston Glacier from the nearly adjoining Quien Sabe and Forbidden Glaciers. Boston Glacier has been in an overall state of retreat since the end of the Little Ice Age around the year 1850. A moderate advance occurred between 1950 and the mid-1970s; however, the retreat resumed and between 1972 and 2006 its terminus retreated 1,470 ft (450 m). See also List of glaciers in the United States References
Challenger Glacier (Washington)

Der Challenger Glacier ist ein Gletscher im North Cascades National Park im US-Bundesstaat Washington am Nordhang des Mount Challenger. Der Gletscher fließt von etwa 8.000 ft (2.438 m) bis auf etwa 5.000 ft (1.524 m) Höhe herab. Mit über 2 mi (3,2 km) Breite endet der Challenger Glacier in einer breiten Zunge mit tiefen Spalten und zahlreichen Eisstürzen und einem Ausläufer im Norden, der in einem Eisstausee endet. Der Aufstieg auf den Gletscher ist eine der am häufigsten gewählten Routen zum Gipfel des Mount Challenger. Weblinks Challenger Glacier. In: Geographic Names Information System. United States Geological Survey, United States Department of the Interior, abgerufen am 31. März 2013 (englisch). Einzelnachweise
Challenger Glacier (Washington)

Challenger Glacier is in North Cascades National Park in the U.S. state of Washington and is on the north slopes of Mount Challenger. Challenger Glacier descends from 8,000 to 5,000 ft (2,400 to 1,500 m). Over 2 mi (3.2 km) wide, Challenger Glacier descends along a wide terminus with heavy crevassing and numerous icefalls, with a tongue of the glacier in the north descending to a proglacial lake. The ascent up Challenger Glacier is one of the most common routes to the summit of Mount Challenger. See also List of glaciers in the United States References
Colchuck-Gletscher

Der Colchuck-Gletscher ist ein Gletscher in der Stuart Range unmittelbar nördlich des Colchuck Peak und des Dragontail Peak im US-Bundesstaat Washington. Der Colchuck-Gletscher liegt in der Alpine Lakes Wilderness des Wenatchee National Forest. Der Gletscher ist etwa 0,30 mi (0,5 km) lang, an der breitesten Stelle 0,10 mi (0,2 km) breit und fließt von 7.600 ft (2.316 m) bis auf 6.400 ft (1.951 m) Höhe herab, wo er auf blankem Fels und in einem Talus endet. Unterhalb des Gletschers befindet sich der Colchuck Lake. Einzelnachweise Weblinks Colchuck Glacier. In: Geographic Names Information System. United States Geological Survey, United States Department of the Interior, abgerufen am 3. März 2013 (englisch).
Colchuck Glacier

Colchuck Glacier is in the Stuart Range immediately north of Colchuck Peak and Dragontail Peak, in the U.S. state of Washington. Colchuck Glacier is within the Alpine Lakes Wilderness of Wenatchee National Forest. The glacier is approximately 0.30 mi (0.48 km) in length, 0.10 mi (0.16 km) in width at its widest and descends from 7,600 to 6,400 ft (2,300 to 2,000 m), where it terminates on barren rock and talus. Below the glacier lies Colchuck Lake. The mountain and glacier take their name from the lake, which in Chinook Jargon means "cold water" or "ice". See also List of glaciers in the United States References
Company Glacier

Der Company Glacier ist ein Gletscher im Wenatchee National Forest im US-Bundesstaat Washington. Er liegt an den Nordhängen des Bonanza Peak, des höchsten nicht-vulkanischen Gipfels der Kaskadenkette. Der Company Glacier fließt von 9.200 ft (2.804 m) bis auf 6.500 ft (1.981 m) in mehreren Hauptrinnen herab, die sich in einer Höhe von 7.800 ft (2.377 m) vereinigen. Der Company Glacier wurde als Zugangsroute beim ersten Aufstieg auf den Bonanza Peak 1937 genutzt. Einzelnachweise Weblinks Company Glacier. In: Geographic Names Information System. United States Geological Survey, United States Department of the Interior, abgerufen am 13. April 2013 (englisch).
Company Glacier

Company Glacier is in Wenatchee National Forest in the U.S. state of Washington, on the north slopes of Bonanza Peak, the tallest non-volcanic peak in the Cascade Range. Company Glacier descends from 9,200 to 6,500 ft (2,800 to 2,000 m) with several main chutes converging into the main glacier below the 7,800-foot (2,400 m) level. Company Glacier was used as the approach route when Bonanza Peak was first climbed in 1937. See also List of glaciers in the United States References
Dana-Gletscher (Washington)

Der Dana-Gletscher liegt im Wenatchee National Forest im US-Bundesstaat Washington, etwa 0,5 mi (1 km) westlich des Dome Peak. Er fließt über eine Strecke von etwa 1,6 Kilometern allgemein nordwärts. Ein Gebirgsgrat teilt den Gletscher in zwei Teile, während weitere Grate ihn vom Chickamin-Gletscher im Osten und vom Dome Glacier im Süden trennen. Der Dana-Gletscher fließt von etwa 8.000 ft (2.438 m) bis auf etwa 6.000 ft (1.829 m) Höhe herab. Einzelnachweise Weblinks Dana Glacier. In: Geographic Names Information System. United States Geological Survey, United States Department of the Interior, abgerufen am 10. März 2013 (englisch).
Dana Glacier (Washington)

Dana Glacier is in Wenatchee National Forest in the U.S. state of Washington and is .50 mi (0.80 km) west of Dome Peak. Dana Glacier flows generally north for a distance of approximately 1 mi (1.6 km). An arête divides the glacier in two while other aretes separate Dana Glacier from Chickamin and Dome Glaciers to the east and south respectively. Dana Glacier descends from nearly 8,000 to 6,000 ft (2,400 to 1,800 m). See also List of glaciers in the United States References
Hinman Glacier

Hinman Glacier was a glacier that flowed to the north and northwest from near the summit of Mount Hinman, in the U.S. state of Washington. Hinman Glacier was within the Alpine Lakes Wilderness of Snoqualmie National Forest. The glacier was approximately 1.3 km2 (320 acres) in 1971, making it the largest glacier between Mount Rainier and Glacier Peak, but an expedition by glaciologists from Nichols College in August 2022 discovered that the glacier had disappeared, with only a few snowfields and non-flowing remnant ice areas totalling 0.04 km2 (9.9 acres) remaining. Smaller glaciers in this part of the Cascade Range preceded the Hinman Glacier in disappearing as part of the retreat of glaciers since 1850 with only three glaciers remaining in King County. History Evidence suggests that Hinman Glacier may have formed as early as the retreat of the Cordilleran ice sheet, which covered the region approximately 14,000 years ago, with it being at least as old as the Mount Mazama eruption 7,000 years ago that created Crater Lake in Oregon. Loss of glacier Made up of two sections, the western lobe was the first to disappear, leaving only small patches of ice by 2009. The glacier persisted on the north flank of Mount Hinman for another decade and repeat photography showed rapid retreat. A new lake, unofficially named Hinman Lake, formed behind the terminal moraine during the second half of the 20th Century as the ice receded. Fragments of the glacier in the form of ice masses are dispersed within and around the lake. In 2023, the glacier was reported to be extinct. Environmental impact Meltwater from Hinman Glacier fed the Skykomish River and in concert with the decline of other glacial ice in this portion of the Cascades, this has led to negative impacts on streamflow of the river and drainage basin into the Puget Sound near Everett. With less dependable late-summer waterflow, measured at approximately 55% surface loss, the depletion can cause harm to Pacific Northwest salmon and other aquatic life in the river, as well as the local population who depend on the waters. See also List of glaciers in the United States References
Isella Glacier

Der Isella Glacier ist ein Gletscher im Wenatchee National Forest im US-Bundesstaat Washington. Er liegt an den Südhängen des Bonanza Peak, des höchsten nicht-vulkanischen Gipfels in der Kaskadenkette. Der Isella Glacier fließt von 8.800 ft (2.682 m) bis auf 7.600 ft (2.316 m) herab. Einzelnachweise Weblinks Isella Glacier. In: Geographic Names Information System. United States Geological Survey, United States Department of the Interior, abgerufen am 13. April 2013 (englisch).
Mary Green Glacier

Der Mary Green Glacier ist ein Gletscher im Wenatchee National Forest im US-Bundesstaat Washington. Er liegt an den Osthängen des Bonanza Peak, des höchsten nicht-vulkanischen Gipfels in der Kaskadenkette. Der Mary Green Glacier fließt von 8.500 ft (2.591 m) bis auf 7.200 ft (2.195 m) herab. Der Mary Green Glacier wurde nach der Frau eines Prospektors benannt und liegt an der beliebtesten Route zum Aufstieg auf den Bonanza Peak. Einzelnachweise Weblinks Mary Green Glacier. In: Geographic Names Information System. United States Geological Survey, United States Department of the Interior, abgerufen am 13. April 2013 (englisch).
Mary Green Glacier

Mary Green Glacier is in Wenatchee National Forest in the U.S. state of Washington, on the east slopes of Bonanza Peak, the tallest non-volcanic peak in the Cascade Range. Mary Green Glacier descends from 8,500 to 7,200 ft (2,600 to 2,200 m). Mary Green Glacier was named after the wife of a prospector and lies along the most popular route to the summit of Bonanza Peak. See also List of glaciers in the United States References
Neve Glacier

Neve Glacier is in North Cascades National Park in the U.S. state of Washington and is on the north slopes of Snowfield Peak. Neve Glacier flows generally north and splits in two with two terminal tongues, one flowing to the northwest which is known as Ladder Creek Glacier and the other descending a total of more than 1.8 mi (2.9 km) to the east. Ladder Creek Glacier descends from 7,800 to 6,000 ft (2,400 to 1,800 m), while the east tongue also originates from the same altitude and descends to 5,600 ft (1,700 m). Between 1850 and 2006, Neve Glacier is estimated to have retreated more than 1,000 m (3,300 ft). See also List of glaciers in the United States Gallery Notes References "Geological Survey Professional Paper 715—A". National Park Service. Retrieved 2017-12-19.
Snow Creek Glacier

Snow Creek Glacier is located on Little Annapurna in the Stuart Range, U.S. state of Washington. Snow Creek Glacier is within the Alpine Lakes Wilderness of Wenatchee National Forest and the Enchantment Lakes region. Snow Creek Glacier consists of several small glacial remnants (glacierets), one of which terminates at Isolation Lake. Snow Creek Glacier is now said to have disappeared. See also List of glaciers in the United States References
West-Nooksack-Gletscher

Der West-Nooksack-Gletscher ist ein Gletscher im North Cascades National Park im US-Bundesstaat Washington. Er liegt an den Osthängen des Mount Shuksan, unmittelbar nordöstlich eines Nebengipfels, des Nooksack Tower. Der West-Nooksack-Gletscher ist nur etwa 0,10 mi (0,16 km) breit; er kann als Überbleibsel der Vergletscherung des Berges betrachtet werden. Das Schmelzwasser des West-Nooksack-Gletschers speist den Nooksack River. Einzelnachweise Weblinks West Nooksack Glacier. In: Geographic Names Information System. United States Geological Survey, United States Department of the Interior, abgerufen am 20. April 2013 (englisch).
West Nooksack Glacier

West Nooksack Glacier is in North Cascades National Park in the U.S. state of Washington, on the eastern slopes of Mount Shuksan, immediately northeast of the subpeak called Nooksack Tower. West Nooksack Glacier is only .10 mi (0.16 km) in length and is a glacial remnant. West Nooksack Glacier provides meltwater for the Nooksack River. See also List of glaciers in the United States References