The mountainous regions that have been glaciated, the valleys are no longer narrow. The ice modifies the valley in three ways: the glacier widens, deepens, and straightens the valley.
Deglaciation is not a feature associated with valley glaciers. Valley glaciers form in mountainous regions due to the accumulation and compaction of snow, creating a flowing mass of ice within a valley. Features associated with valley glaciers include cirques, arêtes, and moraines.
A glaciated mountain valley typically has a U-shaped profile with a broad, flat bottom and steep, straight sides, formed by the movement of glaciers. In contrast, a mountain valley formed through other natural processes, such as erosion from rivers or tectonic activity, may have a V-shaped profile with a narrower bottom and more irregular slopes.
An esker is an elongated landform that is created by the deposition of sediment carried by meltwater streams within or beneath glaciated regions. Eskers are commonly found in areas that have been covered by glaciers in the past.
Alpine glaciers are found in mountain valleys
The two main types of glaciers are alpine glaciers, which form in mountainous regions and flow down valleys, and ice sheets, which are massive continental glaciers that cover large areas of land. Alpine glaciers are smaller and more common, while ice sheets are much larger and thicker.
A landscape which has been carved out by MASSIVE sheets of ice in the period of what is called 'the ice age' (when ice covered a huge % of the earths surface) the movement of this ice cuts through the landscape and forms distinctive features and patterns as they go which geographers and geologists recognise as a glaciated landscape.
The Alps in Europe is a glaciated region known for its numerous glaciers and ice fields. These glaciers have shaped the dramatic landscape and provided valuable water resources to surrounding areas.
An area that has been recently glaciated is most likely to display features such as U-shaped valleys, which are formed as glaciers carve through the landscape. Additionally, one might observe moraines, which are accumulations of debris deposited by glaciers, and fjords, which are deep, narrow inlets created when glaciers retreat. Other features include exposed bedrock and kettle lakes, formed by melting ice blocks.
mountain glaciers
its not mountain glaciers but its valley glaciers
Deglaciation is not a feature associated with valley glaciers. Valley glaciers form in mountainous regions due to the accumulation and compaction of snow, creating a flowing mass of ice within a valley. Features associated with valley glaciers include cirques, arêtes, and moraines.
The small glaciers that exist in high mountainous areas were called mountain glaciers or cirque glaciers.
Yes, fjords, glaciated valleys, and horns are all erosional landforms created by glaciers. Fjords are deep, narrow inlets formed when glaciers retreat and sea levels rise, flooding the valleys they carved. Glaciated valleys, characterized by U-shaping, are formed through the intense erosion by moving ice. Horns are sharp peaks that emerge when multiple glaciers erode a mountain from different sides, creating steep ridges.
Pleistocene glaciers primarily shaped the landscape through processes such as erosion, deposition, and the formation of landforms like moraines and drumlins. They also created features like glacial lakes and valleys. However, a notable effect that Pleistocene glaciers did not have on the landscape is the formation of desert landforms, as their influence was predominantly in cooler, glaciated regions rather than arid environments.
Because glaciers reflect more sunlight back out into space - instead of absorbing it like darker places would,
Alpine glaciers create distinctive features through processes of erosion and deposition. As glaciers move down mountainous terrain, they carve out U-shaped valleys and sharp peaks, known as horns, through abrasion and plucking of rock. Additionally, when glaciers melt, they deposit sediment in the form of moraines, which are ridges of debris left at the glacier's edge. These processes collectively shape the dramatic landscapes characteristic of alpine environments.
The direct geologic effect of glaciers includes the formation of various landforms through processes such as erosion and deposition. Glaciers carve out valleys, create fjords, and shape mountains through their movement, leading to features like U-shaped valleys and cirques. Additionally, as glaciers melt, they deposit sediments, forming moraines, outwash plains, and drumlins, which can significantly alter the landscape. These processes contribute to soil formation and influence ecosystems in glaciated regions.