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Emerald Spring is 27 feet (8.2 m) deep. [5] The water temperature in the spring is around 83.3 °C (181.9 °F). [1] The spring gets its name from the emerald green color of the water created by sunlight filtering through the water, giving the light a blue color, and reflecting off the yellow sulphur creating the green hue.
Norris Hot Springs is 0.4 miles (0.6 km) east of the town, and an agricultural experiment station operated by Montana State University - Bozeman is at Red Bluff, 2.5 miles (4.0 km) east on Highway 84. According to the U.S. Census Bureau, the Norris CDP has an area of 0.34 square miles (0.88 km 2), all of it recorded as land. [1]
Water god in an ancient Roman mosaic. Zeugma Mosaic Museum, Gaziantep, Turkey. A water deity is a deity in mythology associated with water or various bodies of water.Water deities are common in mythology and were usually more important among civilizations in which the sea or ocean, or a great river was more important.
Trail Creek Hot Springs consists of two outdoor walled pools of 116‑degree spring water with valves to let in some cold river water. Just 0.1 miles from the parking area off Highway 55, the ...
Artists' Paintpots is a small hydrothermal area south of Norris Junction that includes colorful hot springs and two large mudpots. The Monument Geyser Basin 44°41′03″N 110°45′14″W / 44.68417°N 110.75389°W / 44.68417; -110.75389 ( Monument Geyser Basin ) has no active geysers, but its 'monuments' are siliceous sinter ...
The Pagosa geothermal hot springs are located on the western slope of the Continental Divide. The sulfur-rich water emerging from what is called the "Mother Spring" has been measured between 110 °F (43 °C) and 144 °F (62 °C). [5] The water originates from 6,000 feet below the surface from volcanic activity. [17]
The hot water that feeds Mammoth comes from Norris Geyser Basin after traveling underground via a fault line [5] 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.
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