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NPS_hot-springs-regional-map.pdf (579 × 456 pixels, file size: 700 KB, MIME type: application/pdf) This is a file from the Wikimedia Commons . Information from its description page there is shown below.
Baker Lake Airport (IATA: YBK, ICAO: CYBK) is located 3 nautical miles (5.6 km; 3.5 mi) southwest of Baker Lake, Nunavut, Canada. It is operated by the government of Nunavut. It has a single gravel runway 4,195 ft × 100 ft (1,279 m × 30 m). [4]
MT 85 travels south from I-90 in Belgrade, providing access to Bozeman Hot Springs. The highway then enters the city of Bozeman, the county seat, and intersects and becomes concurrent with US 191. I-90 exits the county at the Gallatin–Park county border at 5,760-foot (1,760 m) high Bozeman Pass.
Paradise Valley is a major river valley of the Yellowstone River in Southwestern Montana just north of Yellowstone National Park in Park County. The valley is flanked by the Absaroka Range on the east and the Gallatin Range on the west. [1] The Paradise Valley is separated from the Gallatin Valley and Bozeman, MT, by the Bozeman Pass.
This is a dynamic list of hot springs in the United States. The Western states in particular are known for their thermal springs: Alaska, Arizona, California, Colorado, Idaho, Montana, Nevada, New Mexico, Oregon, Utah, Washington, Wyoming; but there are interesting hot springs in other states throughout the country.
Baker Lake Water Aerodrome (TC LID: CJK6) is located at Baker Lake, Nunavut, Canada. The coordinates are for the lake itself; however, there is an alternate landing at Airplane Lake which is located 1.5 nautical miles (2.8 km; 1.7 mi) away from the community.
Under the Nordenskjöld formula for distinguishing polar from non-polar climates, however, Baker Lake's climate is polar (Köppen ET) because with a coldest-month mean of −31.3 °C (−24.3 °F), the warmest-month mean would need be above 12.1 °C (53.8 °F) to keep Baker Lake out of the polar category, while Baker Lake's warmest-month mean ...
The hot springs and seeps are located in the Sevier Desert on Fumarole Butte which is a basaltic andesite type of shield volcano from the Quaternary period, overlaying basalt and rhyolite. [7] The hot water emerges from a travertine and alluvial mound (sometimes described as a tufa mound) that flank the eastern side of the basalt lava formation ...
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