There are glaciers in Pakistan, particularly in the Karakoram and Hindu Kush mountain ranges. However, the number of glaciers is decreasing due to climate change, which is causing them to melt at a faster rate. Environmental factors like temperature increases and changing precipitation patterns are contributing to the retreat of glaciers in Pakistan.
A glacier is often described as a river of ice coming down from a mountain.
At the North Pole, there is no land mass - indeed there has never been a land mass at the North Pole over the past 400 million years - and the pack ice or sea ice that covers the North Pole and surrounding areas is much shallower than the thick glacial ice that covers the South Pole and surrounding areas.
By definition, a thin cover of sea ice is not a glacier since it does not move like a glacier and it is not formed like glaciers are by the accumulation of snowfall. Instead, it forms merely by the freezing of sea water, a process that occurs in winter as far south as Prince Edward Island and Vladivostok in the northern hemisphere.
As a matter of fact, Mount Kosciuszko, which is the highest point in continental Australia, is snow-covered during the winter and spring seasons. It's low height, only 2,228 metres (7,310 ft) above sea level and the warm Australian weather, explain why it isn't snow-covered at other times of year.
The main types of glaciers are valley glaciers, ice caps, ice sheets, piedmont glaciers, outlet glaciers, and cirque glaciers. Valley glaciers form in mountain valleys, ice caps cover smaller areas, ice sheets are massive continental glaciers, piedmont glaciers form at the base of mountains, outlet glaciers are the streams of ice flowing out of ice caps or ice sheets, and cirque glaciers are located in bowl-shaped depressions on mountainsides.
glaciers are very big
its not mountain glaciers but its valley glaciers
Pros:· Glaciers provide drinking water· Glacier water provides plants water· Glaciers help generate hydroelectric powerCons:· Glaciers cause flooding· Glaciers cause avalanches
Advancing glaciers are glaciers that are moving forward and expanding, while retreating glaciers are glaciers that are melting and shrinking. Stationary glaciers are glaciers that are not currently advancing or retreating, maintaining a relatively stable position.
Sachin
Pakistan has almost all kinds of land-forms. The Northern Areas of Pakistan start from highest glaciers, the famous Himalaya range. Pakistan also has plateaus, plains, valleys and deserts. Pakistan also has rivers, streams, and a Arabian sea in the south.
River Indus, without any doubt is the most important river for Pakistan. It's as important for Pakistan as River Nile is for Egypt. River Indus irrigates major areas of Punjab and Sindh. River Indus originates from Glaciers and falls into Arabian Sea near Badin.
The main types of glaciers are valley glaciers, ice caps, ice sheets, piedmont glaciers, outlet glaciers, and cirque glaciers. Valley glaciers form in mountain valleys, ice caps cover smaller areas, ice sheets are massive continental glaciers, piedmont glaciers form at the base of mountains, outlet glaciers are the streams of ice flowing out of ice caps or ice sheets, and cirque glaciers are located in bowl-shaped depressions on mountainsides.
The two most common kinds of glaciers are valley glaciers, which flow down valleys, and ice sheets, which cover extensive areas and can be thousands of meters thick. Valley glaciers are found in mountainous regions, while ice sheets are found in polar regions like Antarctica and Greenland.
Extreme north of Pakistan is full of glaciers and these areas witness very lowest temperatures in winter. The lowest temperature recorded so far was −24.1 °C. This temperature was recorded in 1995 in Sakardu, a town situated in Karakuram Range.
Glaciers formed in mountains are called mountain glaciers or alpine glaciers. They are found in high-altitude regions and flow downhill through valleys.
Continental glaciers are thicker and larger. Valley glaciers are formed on mountains; continental glaciers are formed on flat land.
there are no glaciers in Ireland
glaciers are very big
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.
its not mountain glaciers but its valley glaciers