Livingston Range
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The Livingston Range is a
mountain range A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arise ...
located primarily in Glacier National Park in the
U.S. state In the United States, a state is a constituent political entity, of which there are 50. Bound together in a political union, each state holds governmental jurisdiction over a separate and defined geographic territory where it shares its sove ...
of
Montana Montana () is a state in the Mountain West division of the Western United States. It is bordered by Idaho to the west, North Dakota and South Dakota to the east, Wyoming to the south, and the Canadian provinces of Alberta, British Columb ...
, and in the extreme southeastern section of the
Canadian Canadians (french: Canadiens) are people identified with the country of Canada. This connection may be residential, legal, historical or cultural. For most Canadians, many (or all) of these connections exist and are collectively the source of ...
province of
British Columbia British Columbia (commonly abbreviated as BC) is the westernmost province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, ...
. The range is long and wide. Over 15 summits exceed above sea level, and the highest point is
Kintla Peak Kintla Peak () is a pyramidal peak in the Livingston Range of Glacier National Park in the U.S. state of Montana. It is the tallest mountain in the Livingston Range and the third-tallest in the park. It is also the most northerly peak and land ar ...
at . (While these elevations are not particularly high for North American mountains, they are high compared to the roughly 4,000 foot (1,200 m) elevation of the nearby valleys, making for particularly dramatic peaks.) The Livingston Range was initially uplifted beginning 170 million years ago when the
Lewis Overthrust The Lewis Overthrust is a geologic thrust fault structure of the Rocky Mountains found within the bordering national parks of Glacier in Montana, United States and Waterton Lakes in Alberta, Canada. The structure was created due to the collision o ...
fault pushed an enormous slap of precambrian rocks thick, wide and long over newer rocks of the
cretaceous The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of ...
period.


See also

*
List of mountain ranges in Montana This is a list of mountain ranges in the state of Montana. Montana is the fourth largest state in the United States and is well known for its mountains. The name "Montana" means "mountainous" in Latin. Representative James Mitchell Ashley ( R-Ohi ...
*
Mountains and mountain ranges of Glacier National Park (U.S.) Mountains in Glacier National Park (U.S.) are part of the Rocky Mountains. There are at least 150 named mountain peaks over in Glacier in three mountain ranges--the Clark Range, Lewis Range, Livingston Range. Mount Cleveland at is the high ...


Notes


External links

* * {{Montana Mountain ranges of Montana Mountain ranges of British Columbia Landforms of Glacier County, Montana Glacier National Park (U.S.) Mountains of Glacier National Park (U.S.)