Mammoth Hot Springs (original) (raw)
Mammoth Hot Springs ist der Haupt- und Verwaltungsort des Yellowstone-Nationalparkes in den USA. Seinen Namen verdankt er den nahegelegenen Sinter-Terrassen und heißen Quellen. Er liegt auf 1902 m. ü. M. Nebst den Verwaltungsgebäuden besteht die Ortschaft lediglich aus einem Restaurant, einem Hotel, einem Souvenirladen, einer Tankstelle, einer Kapelle, einem Postbüro sowie aus einigen Häusern und Hütten für Angestellte und Touristen.
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| dbo:abstract | Mammoth Hot Springs ist der Haupt- und Verwaltungsort des Yellowstone-Nationalparkes in den USA. Seinen Namen verdankt er den nahegelegenen Sinter-Terrassen und heißen Quellen. Er liegt auf 1902 m. ü. M. Nebst den Verwaltungsgebäuden besteht die Ortschaft lediglich aus einem Restaurant, einem Hotel, einem Souvenirladen, einer Tankstelle, einer Kapelle, einem Postbüro sowie aus einigen Häusern und Hütten für Angestellte und Touristen. (de) Mammoth Hot Springs - en Esperanto "Mamutaj Varmegaj Fontoj" - estas la ĉefa kaj administra loko de la Nacia Parko Yellowstone en Usono. Sian nomon la loko dankas al la proksimaj kalkoŝtonaj terasoj kaj varmegaj fontoj. Ĝi situas en alteco de 1902 metroj super la marnivelo. Krom la administra konstruaĵo la loĝloko nur konsistas el restoracio, malgranda hotelo, vendejo por suveniroj, benzinejo, kapelo, poŝtoficejo kaj iuj loĝdomoj por parkaj dungitoj kaj turistoj. (eo) Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate (over two tons flow into Mammoth each day in a solution). Because of the huge amount of geothermal vents, travertine flourishes. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas. The hot water that feeds Mammoth comes from Norris Geyser Basin after traveling underground via a fault line that runs through limestone and roughly parallel to the Norris-to-Mammoth road. The limestone from rock formations along the fault is the source of the calcium carbonate. Shallow circulation along this corridor allows Norris's superheated water to slightly cool before surfacing at Mammoth, generally at about 170 °F (80 °C). Algae living in the warm pools have tinted the travertine shades of brown, orange, red, and green. Thermal activity here is extensive both over time and distance. The thermal flows show much variability with some variations taking place over periods ranging from decades to days. Terrace Mountain at Mammoth Hot Springs is the largest known carbonate-depositing spring in the world. The most famous feature at the springs is the Minerva Terrace, a series of travertine terraces. The terraces have been deposited by the spring over many years but, due to recent minor earthquake activity, the spring vent has shifted, rendering the terraces dry. The Mammoth Terraces extend all the way from the hillside, across the Parade Ground, and down to Boiling River. The Mammoth Hotel, as well as all of Fort Yellowstone, is built upon an old terrace formation known as Hotel Terrace. There was some concern when construction began in 1891 on the fort site that the hollow ground would not support the weight of the buildings. Several large sink holes (fenced off) can be seen out on the Parade Ground. This area has been thermally active for several thousand years. The Mammoth area exhibits much evidence of glacial activity from the Pinedale Glaciation. The summit of Terrace Mountain is covered with glacial till, thereby dating the travertine formation there to earlier than the end of the Pinedale Glaciation. Several thermal kames, including Capitol Hill and Dude Hill, are major features of the Mammoth Village area. Ice-marginal stream beds are in evidence in the small, narrow valleys where Floating Island Lake and Phantom Lake are found. In Gardner Canyon one can see the old, sorted gravel bed of the Gardner River covered by unsorted glacial till. (en) Les Mammoth Hot Springs sont un édifice minéral calcaire naturel de type tufière se trouvant dans le parc national de Yellowstone aux États-Unis. Elles sont l'une des principales attractions touristiques de la réserve, après le Old Faithful et le Grand Prismatic Spring. (fr) Le Mammoth Hot Springs sono un sito naturale composto da colline travertino che si sono formate a seguito dell'azione di sorgenti termali: si trovano all'interno del parco nazionale di Yellowstone nelle vicinanze di e del . (it) Mammoth Hot Springs − rozległy kompleks gorących źródeł znajdujący się na trawertynowych wzgórzach w północnej części Parku Narodowego Yellowstone w Wyoming w Stanach Zjednoczonych. W jego bezpośrednim sąsiedztwie znajduje się Fort Yellowstone oraz historyczna osada Mammoth Hot Springs. Kompleks powstawał przez tysiące lat na skutek osadzania się węglanu wapnia wypłukiwanego ze skał przez gorące wody. Źródlane wody, o temperaturze około 80 °C, zawierające także śladowe ilości innych minerałów, schładzając się na powierzchni utworzyły białe, czasem biało-brązowe lub biało-rude nacieki i skorupy, a także efektowne terasy. Barwy tarasów ulegają zmianie w różnych porach roku w zależności od intensywności wypływania wody a także od rodzaju glonów i sinic znajdujących się w wodzie. (pl) 猛犸温泉（Mammoth Hot Springs）是美國黃石國家公園洞石上的一个大型溫泉综合体，它毗邻以及。猛犸温泉是随着数千年来热泉水的不斷冷却和碳酸鈣沉积而形成的。 (zh) |
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| rdfs:comment | Mammoth Hot Springs ist der Haupt- und Verwaltungsort des Yellowstone-Nationalparkes in den USA. Seinen Namen verdankt er den nahegelegenen Sinter-Terrassen und heißen Quellen. Er liegt auf 1902 m. ü. M. Nebst den Verwaltungsgebäuden besteht die Ortschaft lediglich aus einem Restaurant, einem Hotel, einem Souvenirladen, einer Tankstelle, einer Kapelle, einem Postbüro sowie aus einigen Häusern und Hütten für Angestellte und Touristen. (de) Mammoth Hot Springs - en Esperanto "Mamutaj Varmegaj Fontoj" - estas la ĉefa kaj administra loko de la Nacia Parko Yellowstone en Usono. Sian nomon la loko dankas al la proksimaj kalkoŝtonaj terasoj kaj varmegaj fontoj. Ĝi situas en alteco de 1902 metroj super la marnivelo. Krom la administra konstruaĵo la loĝloko nur konsistas el restoracio, malgranda hotelo, vendejo por suveniroj, benzinejo, kapelo, poŝtoficejo kaj iuj loĝdomoj por parkaj dungitoj kaj turistoj. (eo) Les Mammoth Hot Springs sont un édifice minéral calcaire naturel de type tufière se trouvant dans le parc national de Yellowstone aux États-Unis. Elles sont l'une des principales attractions touristiques de la réserve, après le Old Faithful et le Grand Prismatic Spring. (fr) Le Mammoth Hot Springs sono un sito naturale composto da colline travertino che si sono formate a seguito dell'azione di sorgenti termali: si trovano all'interno del parco nazionale di Yellowstone nelle vicinanze di e del . (it) Mammoth Hot Springs − rozległy kompleks gorących źródeł znajdujący się na trawertynowych wzgórzach w północnej części Parku Narodowego Yellowstone w Wyoming w Stanach Zjednoczonych. W jego bezpośrednim sąsiedztwie znajduje się Fort Yellowstone oraz historyczna osada Mammoth Hot Springs. Kompleks powstawał przez tysiące lat na skutek osadzania się węglanu wapnia wypłukiwanego ze skał przez gorące wody. Źródlane wody, o temperaturze około 80 °C, zawierające także śladowe ilości innych minerałów, schładzając się na powierzchni utworzyły białe, czasem biało-brązowe lub biało-rude nacieki i skorupy, a także efektowne terasy. Barwy tarasów ulegają zmianie w różnych porach roku w zależności od intensywności wypływania wody a także od rodzaju glonów i sinic znajdujących się w wodzie. (pl) 猛犸温泉（Mammoth Hot Springs）是美國黃石國家公園洞石上的一个大型溫泉综合体，它毗邻以及。猛犸温泉是随着数千年来热泉水的不斷冷却和碳酸鈣沉积而形成的。 (zh) Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate (over two tons flow into Mammoth each day in a solution). Because of the huge amount of geothermal vents, travertine flourishes. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas. (en) |
| rdfs:label | Mammoth Hot Springs (de) Mammoth Hot Springs (eo) Mammoth Hot Springs (en) Mammoth Hot Springs (fr) Mammoth Hot Springs (it) Mammoth Hot Springs (pl) 猛犸温泉 (zh) |
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