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  2. Pulled by gravity, an alpine glacier moves slowly down a valley. Some glaciers, called hanging glaciers, don't flow the entire length of a mountain. Avalanches and icefalls transfer glacial ice from hanging glaciers to a larger glacier beneath them, or directly to the valley below. An ice sheet spreads out from its center.
    education.nationalgeographic.org/resource/glacier-moving-rivers-ice/
    education.nationalgeographic.org/resource/glacier-moving-rivers-ice/
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    How do alpine glaciers flow?The flow of alpine glaciers is primarily controlled by the slope of the land beneath (Figure 4.2.4). In the zone of accumulation the rate of snowfall is greater than the rate of melting. In other words, not all of the snow that falls each winter melts during the following summer, and the ice surface is always covered with snow.
    What is an alpine glacier called?Alpine glaciers, also known as mountain glaciers or cirque glaciers, form on the crests and slopes of mountains. An alpine glacier that fills a valley is sometimes called a valley glacier. A large body of glacial ice astride a mountain, mountain range, or volcano is termed an ice cap or ice field.
    What is an alpine glacier that fills a valley called?An alpine glacier that fills a valley is sometimes called a valley glacier. A large body of glacial ice astride a mountain, mountain range, or volcano is termed an ice cap or ice field. Ice caps have an area less than 50,000 km² (20,000 mile²) by definition.
    What are the two types of glaciers?A glacier is an accumulation of ice and snow that slowly flows over land. There are two main categories of glaciers: alpine glaciers and ice sheets. Alpine glaciers are frozen rivers of ice, slowly flowing under their own weight down mountainsides and into valleys.
     
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