i believe that you are talking about glacial striations
They are called glacial striations. These marks are created by the abrasion of rocks and sediment as a glacier moves over them, leaving parallel grooves and scratches on the surface of the rock.
When glaciers move, they pick up rocks of various sizes. These rocks are then dragged along the bedrock beneath the glacier, causing abrasion. The rocks act like sandpaper, scraping and carving grooves and scratches into the bedrock as the glacier advances.
Glacial grooves are striations or scratches left on rock surfaces as glaciers move over them. The orientation and alignment of these grooves indicate the direction of the glacier's flow, as they are created by the movement of debris embedded in the glacier's base. By analyzing the pattern and angle of the grooves, geologists can determine the glacier's path and the dynamics of its movement during its advance and retreat.
Plucking is a process where glaciers erode the underlying bedrock by freezing onto rocks and pulling them away as the glacier moves. This action creates grooves and scratches in the bedrock, known as glacial striations. These markings serve as evidence of the glacier's movement and direction, providing valuable information about past glacial activity. Ultimately, plucking contributes to the overall shaping of the landscape by carving out features such as valleys and fjords.
Plucking is a process where glaciers erode bedrock by lifting and removing chunks of rock as they move. As the glacier advances, the pressure and movement cause rocks to fracture and break away from the underlying bedrock. This action creates distinctive grooves and scratches, known as striations, which provide evidence of the glacier's flow direction. Such features are commonly observed in glacial landscapes and are important for understanding past glacial activity.
Striations
They are called glacial striations. These marks are created by the abrasion of rocks and sediment as a glacier moves over them, leaving parallel grooves and scratches on the surface of the rock.
A glacier produces grooves and scratches.
Drag loose rocks over Earth's surface
"Starration " is not a word in English language. You may mean 'striation' which is one of multiple, usually parallel grooves or scratches on a material's surface
stria
Glacier grooves are long, parallel scratches or striations on bedrock surfaces that are formed by the movement of glaciers. As a glacier flows over rocky surfaces, it picks up rock fragments and debris, which then act like sandpaper, carving long, linear grooves into the bedrock. These grooves provide valuable insight into the direction and extent of past glacial movements.
By the passing by of a glacier.
Glacial grooves are long, parallel scratches or gouges on bedrock caused by the movement of rocks and debris trapped in the base of a glacier. They are formed as the glacier advances and retreats, grinding the underlying rock surface as it moves. Glacial grooves provide valuable information about the direction and extent of past glacial movements.
When glaciers move, they pick up rocks of various sizes. These rocks are then dragged along the bedrock beneath the glacier, causing abrasion. The rocks act like sandpaper, scraping and carving grooves and scratches into the bedrock as the glacier advances.
glacial ice
On rocks - they are the parallel groves or scratches. Or on skeletal or cardiac muscle: they are the "strands" of the muscle.