the direction of glacial movement 🥶
the direction of glacial movement 🥶
Furrows of glacial origin in bedrock that are deeper and wider than striations- Double S
Striations are "scratches" left in bedrock by glaciers. A small particle of rock, generally pebble sized or smaller, becomes entrained in the base of the glacier and dragged along the surface of the bedrock. These can often be seen on hard bedrock surfaces that are resistant to subsequent weathering after the retreat of the glacier. Erratics are large rocks that are found out of place in the landscape, i.e. not near where they were formed. They are removed from their provenance by a glacier and transported away, before being deposited in a different part or the landscape when the glacier melts.
glacial movement
Abrasion
the direction of glacial movement 🥶
The gouging of bedrock by rock fragments dragged by glaciers results in the formation of grooves, scratches, and striations on the surface of the bedrock. These features, known as glacial striations, provide evidence of the direction and movement of past glaciers. These marks can also help geologists determine the extent and timing of glacial activity in an area.
Furrows of glacial origin in bedrock that are deeper and wider than striations- Double S
Striations are "scratches" left in bedrock by glaciers. A small particle of rock, generally pebble sized or smaller, becomes entrained in the base of the glacier and dragged along the surface of the bedrock. These can often be seen on hard bedrock surfaces that are resistant to subsequent weathering after the retreat of the glacier. Erratics are large rocks that are found out of place in the landscape, i.e. not near where they were formed. They are removed from their provenance by a glacier and transported away, before being deposited in a different part or the landscape when the glacier melts.
U-shaped valleys, erratic boulders and rocks, modern soils, glacial striations on bedrock, the Great Lakes in the United States, extinction events, and massive redistribution of soils and rock.
striations
Glacial Erratic.
An area of land where the bedrock is exposed is referred to by geologists as a bedrock outcrop.
glacial movement
Abrasion
Glacial grooves are caused by the ice picking up boulders and scraping them across the bedrock.
Glacial grooves are caused by the ice picking up boulders and scraping them across the bedrock.