Antarctica is a continental glacier. Alpine glaciers are a different type of glacier.
They difference between them is where there flow. Continental glaciers are enormous ice sheets, and are found in Greenland and Antarctica. Alpine glaciers form in mountain valleys.
Antarctica is about as large as USA and Mexico, combined. Ninety-eight percent of it is covered with an ice sheet containing innumerable glaciers.
The alpine glaciers are high in the mountains.
There are no rivers in Antarctica, it is covered in ice. There are a few glaciers.
Glaciers formed in mountains are called mountain glaciers or alpine glaciers. They are found in high-altitude regions and flow downhill through valleys.
There are 2 main types of glaciers, Continental is one, they float away from central regions. The second is alpine or valley which are the glaciers that flow down the valley from the mountain.
Antarctica's ice cap covers Antarctica and is the biggest ice pack on Earth. It covers 98% of the land on Antarctica and holds 30 million cubic kilometers of ice, enough to raise the world's sea levels by 70 meters if it melted. In East Antarctica the ice rests on land, but in West Antarctica the ice rests on rock sometimes two and a half kilometers (more than 1.5 miles) below sea level. The weight of the ice has actually lowered the surface of the bedrock. Snow falls on Antarctica, and the weight of the snow above turns it to ice. This ice is continually pushed outwards, sometimes with the help of fast moving glaciers, till it reaches the sea, where it floats out, eventually breaking off and forming icebergs (calving) which eventually melt. This process is how the water cycle works in Antarctica.
Alpine glaciers are smaller in size and are found in mountainous regions, while continental glaciers cover much larger areas of land. Alpine glaciers move down valleys, while continental glaciers flow outwards in all directions from a central ice dome. Alpine glaciers are influenced by local topography and weather conditions, while continental glaciers are influenced by global climate patterns. Alpine glaciers tend to have higher melt rates due to their lower elevation compared to continental glaciers. Alpine glaciers are more accessible for study and research compared to the remote and harsh environments of continental glaciers.
The two major types of glaciers are alpine glaciers and continental glaciers. Alpine glaciers, also known as mountain glaciers, are found in mountainous regions and flow down valleys, such as those in the Rocky Mountains and the Himalayas. Continental glaciers, or ice sheets, cover vast areas of land and are found in places like Antarctica and Greenland. Both types play significant roles in shaping landscapes and influencing global sea levels.
Antarctica has many landforms such as:glacierdesertmountainplainplateauvalleynunatakAnother AnswerBe aware that glaciers, desert, plain, plateau and valley are generally covered with ice.
All of Antarctica is covered with an ice sheet, which represents 90% of the earth's store of ice. The list of glaciers includes hundreds of names from the Aagaard Glacier to the Zykov Glacier with the Beardmore and the Recovery in between.