Definition:
An alpine type of glacier is a large mass of ice that forms in high mountain valleys and moves downwards due to gravity. These glaciers are usually found in mountainous regions where the temperature is cold enough for snow to accumulate and turn into ice.
In scientific discussions, you might encounter terms related to the study of alpine glaciers, such as "glaciology" (the study of glaciers) or "moraine" (the debris left behind by a glacier).
While there are no specific idioms or phrasal verbs directly related to "alpine type of glacier," you might use phrases like: - "On thin ice" to describe a risky situation, which metaphorically relates to glaciers and ice. - "To break the ice," which means to start a conversation in a social setting, drawing on the idea of ice as a barrier.
An alpine type of glacier is a glacier that forms in high valleys and moves downward. You can use this term to discuss specific types of glaciers in a geographic or environmental context.