Final answer:
Alpine Glaciers are found in high-altitude locations, forming where temperatures allow snow accumulation in mountain ranges. They are distinct from continental glaciers as they are smaller and confined to mountainous areas. Glacier National Park is an example of alpine glaciation.
Step-by-step explanation:
The type of glacier that can be found in high-altitude locations is the Alpine Glacier. Alpine glaciers are found in mountain ranges around the world and are also known as mountain glaciers. They form in high-altitude areas where temperatures are low enough to allow for the accumulation of snow, which eventually compacts and turns to ice. These glaciers flow down valleys and are much smaller than ice sheets or continental glaciers.
Examples of alpine glaciation can be seen in the Rocky Mountains, the Himalayas, the Alps, and other high-mountain regions. Alpine Glaciers are key indicators of climate change as they are sensitive to changes in temperature and precipitation.
Continental glaciers are different from Alpine Glaciers as they cover much larger areas and are not confined to mountainous regions. Ice sheets, like those found in Antarctica or Greenland, are a type of continental glacier.
To illustrate, Glacier National Park in Montana, USA, features a range of glaciers that have formed over time due to sufficient snowfall accumulation. These glaciers characterize the dynamic nature of alpine environments and shape the landscape through processes like erosion and deposition.