The Flatiron is the name for an

eroded Erosion is the action of surface processes (such as Surface runoff, water flow or wind) that removes soil, Rock (geology), rock, or dissolved material from one location on the Earth's crust#Crust, Earth's crust, and then sediment transport, tra ...

volcanic A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates a ...

outcrop An outcrop or rocky outcrop is a visible exposure of bedrock or ancient superficial deposits on the surface of the Earth. Features Outcrops do not cover the majority of the Earth's land surface because in most places the bedrock or superficial ...

in east-central

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, ...

, Canada, located in

Wells Gray Provincial Park Wells Gray Provincial Park is a large wilderness park located in east-central British Columbia, Canada. The park protects most of the southern, and highest, regions of the Cariboo Mountains and covers 5,250 square kilometres (524,990 hectares or ...

.Catalogue of Canadian volcanoes: Flatiron
The Flatiron is high, long and generally about wide. It is flanked by Hemp Creek to the west and Trout Creek to the east.Neave, Roland (2015). ''Exploring Wells Gray Park'', 6th edition. Wells Gray Tours, Kamloops, BC. .

Geology

About 200,000 years ago, a lake formed in the Hemp Canyonlands with its upper end near the meeting of Trout and Hemp creeks. The lake bottom was about above the present bottom of the Hemp Creek Valley. The surface of the lake was the rim of the Hemp cliffs a few kilometres south of The Flatiron. The lake was created by a blockage downstream on the Clearwater River, but its actual location is unknown, and this could have been an ice dam, a landslide or a lava flow. The Flatiron erupted into this lake and was once much bigger than today. This action is called a ponded lava flow. The lava used to extend right across the Hemp Creek Valley, but floods from melting glaciers carried away the lava and left The Flatiron as a remnant. The water flow might have been 100 times the size of Hemp Creek today. The lava that is exposed today cooled very slowly and formed into columns, one of the park’s finest examples of

columnar basalt Basalt (; ) is an aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the surface of a rocky planet or moon. More than 90% of a ...

. The columns that make up the Flatiron have been falling away regularly and piling up at the base, so the Flatiron keeps gets thinner.

Access

A one-hour hike from Clearwater Valley Road (also called Wells Gray Park Road) leads to a viewpoint of the Hemp Canyonlands with the Flatiron in the distance. After another 30 minutes hiking, it is necessary to leave the trail and bushwhack to the base of the Flatiron. As the cliffs almost surround the Flatiron, the only access to the top is a scramble from the west side above Hemp Creek.

References

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Geology

Access

References

See also