Answer: Option D
Explanation:
The continental glaciation are the continuous masses of the ice that are much larger than the alpine glaciers.
The small continental glacier are called the ice fields an the big Continental glaciers are known as the ice sheets.
Some of the examples of continental glaciers are drumlins, kames, eskers et cetera. These continents are of various shapes and sizes, some are of dome shapes. Some of them are quite bog and some of them are quite small.
