Valley glaciers flow down mountain slopes... so they flow down. I finally found this answer in a book.
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.
Glaciers can move in any direction, including backwards, but typically they move in the direction of their accumulating mass (downhill). Factors such as changes in temperature, pressure, and topography can influence the direction of glacier movement.
in all directions
Valleys are formed by glaciers through a process called glacial erosion. As glaciers move, they pick up rocks and debris, which act as tools to scrape and carve the underlying bedrock. Over time, this erosion deepens and widens the valley, creating the distinctive U-shape commonly associated with glacial valleys.
No. Valley glaciers are a few miles to a few tens of miles long. Continental glaciers are hundreds to thousands of miles long.
A continental glacier can move in all directions and a valley glacier can move in a surge. :)
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.
they went north
A long narrow glacier that forms between mountains is called a valley glacier. These glaciers flow down valleys, eroding the surrounding landscape as they move. Valley glaciers are common in mountainous regions around the world.
Glaciers are big chucks of ice that are usually seen at the north and south pole. The glacier's move in the direction of the waters current.
Glaciers can move in any direction, including backwards, but typically they move in the direction of their accumulating mass (downhill). Factors such as changes in temperature, pressure, and topography can influence the direction of glacier movement.
in all directions
Continental glaciers are thicker and larger. Valley glaciers are formed on mountains; continental glaciers are formed on flat land.
valley glaciers
Valleys are formed by glaciers through a process called glacial erosion. As glaciers move, they pick up rocks and debris, which act as tools to scrape and carve the underlying bedrock. Over time, this erosion deepens and widens the valley, creating the distinctive U-shape commonly associated with glacial valleys.
It is valley and continental glaciers they are different because continental glaciers are the largest, and valley glaciers are on the top of mountain peaks.
Continental glaciers and valley glaciers are both types of glaciers that form from accumulated snowfall. They both flow under the influence of gravity, albeit in different directions. While continental glaciers cover vast areas like an ice sheet, valley glaciers are confined to mountain valleys and flow down through them.