0
What else can I help you with?
Which is not a feature associated with 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.
How does the shape of the glaciated mountain valley differ from the mountain valley?
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.
What is an elongated landform produced when glaciers move over older moraines?
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 can be found on which landform?
Alpine glaciers are found in mountain valleys
What are the two kinds of glaciers and how are they different?
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.
What is a glaciated landscape?
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.
What is one glaciated region?
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.
What are the small glaciers that exist in high mountainous areas?
mountain glaciers
The small glaciers that exist in high mountainous areas are called?
its not mountain glaciers but its valley glaciers
Which is not a feature associated with 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 mountain areas are called what?
The small glaciers that exist in high mountainous areas were called mountain glaciers or cirque glaciers.
Why is it colder in glaciated places?
Because glaciers reflect more sunlight back out into space - instead of absorbing it like darker places would,
Is Svalbard flat or rocky?
Svalbard is very mountainous with lots of glaciers and fjords.
Explain the cause and effect of glaciers in New York?
it made places for large buildings to take place. that's where they make large buildings, on to of glaciated places
How can you tell whether valley glaciers once existed in a mountainous region?
Look at the shape of the valleys. If they are V-shaped there were no valley glaciers; if they are U-shaped there were.
How does the shape of the glaciated mountain valley differ from the mountain valley?
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.
What are some differences in how two types of glaciers affect the land?
There are two primary types of glaciers: alpine glaciers and continental glaciers. Alpine glaciers, found in mountainous regions, carve sharp, U-shaped valleys and create features like cirques and arêtes as they move down slopes. In contrast, continental glaciers, which cover vast land areas like Greenland and Antarctica, reshape the landscape on a much larger scale, flattening terrain and depositing thick layers of sediment, resulting in features like drumlins and moraines. While both types of glaciers erode and transport material, their impacts on the land differ significantly due to their sizes and environments.
