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What is a deposit of loose material carried and left by a glacier and sounds like terrain?
moraine
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What is a deposit of loose material carried and left by a glacier sounds like terrain?
A deposit of loose material carried and left by a glacier is known as moraine. Moraines can vary in size and composition, and they are typically found in areas where glaciers have advanced or retreated. They can include rocks, sand, gravel, and other debris that the glacier has picked up and transported.
What is a deposit of loose material carried and left by a glacier which rhymes with the word terrain?
Moraine. .....hah this is from the same wordsearch im doing......hahaha lol yah im doing it too
Crevasses are gaping cracks that form in the upper part of a glacier Why do crevasses form?
Brittle ice breaks as the glacier crosses rough terrain
What matierial did they use in the aqueducts?
The materials used in aqueducts would depend upon the terrain that the aqueduct crossed. However the piping that actually carried the water was made of a ceramic material. The pipes that led from the aqueduct to the baths, fountains and houses were made of lead.The materials used in aqueducts would depend upon the terrain that the aqueduct crossed. However the piping that actually carried the water was made of a ceramic material. The pipes that led from the aqueduct to the baths, fountains and houses were made of lead.The materials used in aqueducts would depend upon the terrain that the aqueduct crossed. However the piping that actually carried the water was made of a ceramic material. The pipes that led from the aqueduct to the baths, fountains and houses were made of lead.The materials used in aqueducts would depend upon the terrain that the aqueduct crossed. However the piping that actually carried the water was made of a ceramic material. The pipes that led from the aqueduct to the baths, fountains and houses were made of lead.The materials used in aqueducts would depend upon the terrain that the aqueduct crossed. However the piping that actually carried the water was made of a ceramic material. The pipes that led from the aqueduct to the baths, fountains and houses were made of lead.The materials used in aqueducts would depend upon the terrain that the aqueduct crossed. However the piping that actually carried the water was made of a ceramic material. The pipes that led from the aqueduct to the baths, fountains and houses were made of lead.The materials used in aqueducts would depend upon the terrain that the aqueduct crossed. However the piping that actually carried the water was made of a ceramic material. The pipes that led from the aqueduct to the baths, fountains and houses were made of lead.The materials used in aqueducts would depend upon the terrain that the aqueduct crossed. However the piping that actually carried the water was made of a ceramic material. The pipes that led from the aqueduct to the baths, fountains and houses were made of lead.The materials used in aqueducts would depend upon the terrain that the aqueduct crossed. However the piping that actually carried the water was made of a ceramic material. The pipes that led from the aqueduct to the baths, fountains and houses were made of lead.
What is a crevasse in a glacier and how does it form?
A crevasse in a glacier is a deep crack or fissure that forms in the ice due to stress and movement. It is typically caused by the glacier's flow over uneven terrain or changes in speed. Crevasse formation can also be influenced by factors such as temperature changes and the glacier's internal structure.
What is a crevasse at the head of a mountain glacier called?
A crevasse at the head of a mountain glacier is called a "bergschrund." This feature typically forms where the glacier begins to separate from the surrounding terrain, often due to differential movement between the glacier and the mountain slope. Bergschrunds can be quite deep and wide, posing challenges for climbers and hikers navigating the glacier.
What are the cracks in the ice that forms a glacier?
The cracks in an ice glacier are called crevasses. They form due to the movement of the glacier over uneven terrain, causing the ice to fracture and crack. Crevasses can be dangerous to climbers and hikers as they can be deep and difficult to see.
Fissure or deep cleft in glacial ice?
A crevasse is a deep crack or fissure in a glacier ice. It forms when the glacier moves over uneven terrain or when it is subjected to shearing stresses. Crevasse fields can be dangerous to navigate and require careful glacier travel techniques.
What kind of terrain and landform would indicate the prior existence of a continental glacier?
When the glacier melted from North America it left a mass of "heterogeneous" rock debris (loosely termed "glacial drift") etc
What kind of terrain and landforms would indicate the prior existence of continental glacier?
When the glacier melted from North America it left a mass of "heterogeneous" rock debris (loosely termed "glacial drift") etc
Why are the uppermost 50 meters of a glacier referred to as the zone of fracture?
The zone of fracture experiences tension hen the glacier moves over irregular terrain. This tension results in gaping cracks called crevasses. Crevasses can be 50 meters deep. They are often hidden by snow and make travel across glaciers dangerous.
What kind of terrain and landforms would indicate the prior existence a valley glacier?
The presence of U-shaped valleys, which are often wider and deeper than river valleys, indicates the former existence of a valley glacier. Other landforms such as moraines, which are accumulations of debris deposited by the glacier, and cirques, which are bowl-shaped depressions at the glacier's head, also suggest glacial activity. Additionally, features like fjords or hanging valleys can provide evidence of glacial erosion. Scratched and polished bedrock surfaces, known as glacial striations, further indicate the movement of a glacier across the terrain.
