|Elevation||12,807 ft (3,904 m)|
BEARTOOTH MOUNTAINS Latitude and Longitude:
|States||Montana and Wyoming|
|Parent range||Rocky Mountains|
The Beartooth Mountains are located in south central Montana and northwest Wyoming, U.S. and are part of the 900,000 acre (3,600 km2) Absaroka-Beartooth Wilderness, within Custer, Gallatin and Shoshone National Forests. The Beartooths are the location of Granite Peak, which at 12,807 feet (3,904 m) is the highest point in the state of Montana. The mountains are just northeast of Yellowstone National Park  and are part of the Greater Yellowstone Ecosystem. The mountains are traversed by road via the Beartooth Highway (U.S. 212) with the highest elevation at Beartooth Pass (10,947 ft, 3,345 m). The name of the mountain range is attributed to a rugged peak found in the range, Beartooth Peak, that has the appearance of a bear's tooth.
The Beartooth Mountains sit upon the larger Beartooth Plateau, the largest true high elevation plateau in the United States.
The remoteness of the region contributed to their obscurity until the 1870s. The Crow tribe of Native Americans used the valleys of the mountains for hunting game animals and for winter shelter from the harsh winds of the plains. Though trappers entered the region in the 1830s, formal exploration by the U.S. Government did not occur until 1878. Since then, almost 400 species of plants have been discovered and the Beartooths are considered to be the most biologically unique mountain range in North America. The region is also home to one of the largest populations of grizzly bears outside of Alaska and Canada. Black bears, mountain goats, bighorn sheep, elk, moose, wolverine, mountain lion, and lynx are also found here.
Since 2000 the wolf has also reappeared from the migration of wolves that were transplanted into neighboring Yellowstone National Park from Canada. Primarily plants and grasses exist above the 9,000 foot (2,700 m) timberline and Engelmann spruce, subalpine fir, whitebark pine, and lodgepole pine are found below.
The Beartooth mountains are composed of Precambrian granite and crystalline metamorphic rocks dated at approximately 4 to 2.7 billion years old, making these rocks among the oldest on Earth. The Stillwater igneous complex within the mountains is the location of the largest known deposits of platinum and chromium and the second largest deposits of nickel found in the United States. Older ages (4-3.2 billion years) are found in zircon crystals in meta-sedimentary rocks. The most abundant rocks in the Beartooths ( gneiss, amphibolites and granites, as well as the Stillwater Complex) are 2.9-2.7 billion years old. 
Huge expansive plateaus are found at altitudes in excess of 10,000 ft (3,000 m) with over 25 peaks exceeding 12,000 ft (3,700 m). The mountains have over 300 pristine lakes and some waterfalls in excess of 300 feet (91 m). Winters are severe with heavy snow and incessant winds. Approximately 25 small glaciers exist in the Beartooths with Grasshopper Glacier being one of the more distinctive.
The highest peaks of the Beartooth Mountains are clustered in three groups, topped by Granite Peak, Mount Wood 12,649 ft (3,855 m), and Castle Mountain 12,617 ft (3,846 m). The cluster containing Mount Wood is named the Granite Range.  The largest of these three contiguous areas above 10,000 feet (3,000 m), which extends into Wyoming, is the one dominated by Castle Mountain.
BEARTOOTH MOUNTAINS INFORMATION
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