Valley glaciers are formed in high altitudes (e.g. mountains) and continental glaciers are formed in high latitudes (e.g. Greenland). Therefore, they both cover land areas but continental glaciers generally cover more area.
Two types of glaciers are valley glaciers, which flow down valleys, and ice sheets, which cover large land areas. Valley glaciers are narrower and are found in mountainous regions, while ice sheets are massive and cover extensive areas.
The geography of the Anchroage area won't support a Piedmont glacier. This glacier (the Piedmont glacier) is characterized by large stagnant ice sheets where a glacier or glaciers "doesn't/don't have anywhere to go" for lack of an outlet. All the areas around Anchroage, Alaska slope down to the sea. There is no place for the ice of a Piedmont glacier to "build up" for lack of a way to "break out" or to "get stopped" to form this glacier.
Continental and valley glaciers both develop in regions where there is constant snowfall and freezing temperatures throughout the year. Both types of glaciers move at a very slow pace.
Size and location. Valley glaciers are smaller, flowing down valleys in mountainous regions, while ice sheets are vast expanses of ice covering large land areas like the Antarctic and Greenland ice sheets.
Kames. Many are found in areas of kettles and moraines.
A U-shaped valley is a geological formation formed by the erosive action of a glacier. Ice moving downhill carves out a broad, U-shaped valley with steep sides and a flat bottom. These valleys are characteristic of areas that have been shaped by glacier activity.
Two types of glaciers are valley glaciers, which flow down valleys, and ice sheets, which cover large land areas. Valley glaciers are narrower and are found in mountainous regions, while ice sheets are massive and cover extensive areas.
The geography of the Anchroage area won't support a Piedmont glacier. This glacier (the Piedmont glacier) is characterized by large stagnant ice sheets where a glacier or glaciers "doesn't/don't have anywhere to go" for lack of an outlet. All the areas around Anchroage, Alaska slope down to the sea. There is no place for the ice of a Piedmont glacier to "build up" for lack of a way to "break out" or to "get stopped" to form this glacier.
a. deepens itb. straightens itc. all of thesed. only deepens it and widens itC.) all of these
Continental and valley glaciers both develop in regions where there is constant snowfall and freezing temperatures throughout the year. Both types of glaciers move at a very slow pace.
Size and location. Valley glaciers are smaller, flowing down valleys in mountainous regions, while ice sheets are vast expanses of ice covering large land areas like the Antarctic and Greenland ice sheets.
Erosional features in areas with valley glaciers include U-shaped valleys, cirques (bowl-shaped hollows at the head of glaciers), arêtes (sharp ridge between cirques), and hanging valleys (smaller valleys that join a main glacier valley). Glacial striations (scratches on bedrock caused by moving glacier ice) and moraines (piles of debris deposited by glaciers) are also common erosional features.
Kames. Many are found in areas of kettles and moraines.
Continental glaciers are vast sheets of ice that cover large land areas, while valley glaciers are elongated glaciers that flow down mountain valleys. Continental glaciers are typically found in polar regions and cover large portions of Antarctica and Greenland, while valley glaciers are common in mountainous regions worldwide.
An ice cap glacier is a dome-shaped glacier that flows in all directions from a central high point. These glaciers cover large areas and can have multiple outlet glaciers flowing towards different directions.
Yes, there is a glacier on the summit of Cotopaxi, an active stratovolcano in Ecuador. The glacier is receding due to climate change and volcanic activity, posing potential hazards to surrounding areas. Efforts are being made to monitor the glacier and its impacts on the region.
A continental glacier is a glacier that spreads out from a central mass of ice.Hope this helps.Answer 2:A continental glacier is a an ice sheet covering much of a continent