page_title: Mount Torment
section_title: Geology
hierarchical_section_title: Mount Torment / Geology
caption_attribution_description: English: Forbidden Peak (center skyline); Mount Torment (left, middle distance, double summit with snow; Mount Logan (near left edge, skyline, beyond snow-filled saddle at the upper margin of Boston Glacier) Viewpoint location: Hidden Lake Trail, North Cascades National Park Viewpoint elevation: 1792 meter (5878 ft) View direction: 80° Location source: Garmin GPSmap 60CSx Location Datum: WGS84
context_page_description: Mount Torment is a 8,120+ -foot high peak in the North Cascades of Washington in the United States. It is located approximately 65 miles northeast of the city of Everett. First ascended on August 23, 1946, its name originates from the first ascent party, because of "the torture of a hot day with only one orange for quenching thirst." Since then, Mount Torment has gained popularity because of the Torment-Forbidden Traverse to neighboring Forbidden Peak, an exposed alpine route.
  The North Fork Cascade River rises in a basin below Mount Torment and flows several miles west to the Cascade River. Numerous waterfalls are found in this valley.
context_section_description: The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks, spires, ridges, and deep glacial valleys. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to various climate differences.
  The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch. With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted.  In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.
  During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris. The "U"-shaped cross section of the river valleys are a result of recent glaciation. Uplift and faulting in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North Cascades area.
caption: Mount Torment below left of Forbidden Peak (center)
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