Closed depressions occur in both glacial and karst regions, but how do their causes differ?
Answer and explanation
Correct answer: Glacial hollows may relate to melting ice or deposits, while karst hollows form by solution or collapse
The governing distinction is the geomorphic agent. In glacial terrain, a kettle hollow may form when buried stagnant ice melts, or depressions may be associated with glacial deposits and erosion. In karst terrain, soluble limestone is removed by groundwater, producing depressions such as dolines; collapse can enlarge them. Option A correctly contrasts these causes, whereas the other options wrongly assign one agent to both environments.
Frequently asked questions
What is the correct answer to this question?
Glacial hollows may relate to melting ice or deposits, while karst hollows form by solution or collapse
Why is this the correct answer?
The governing distinction is the geomorphic agent. In glacial terrain, a kettle hollow may form when buried stagnant ice melts, or depressions may be associated with glacial deposits and erosion. In karst terrain, soluble limestone is removed by groundwater, producing depressions such as dolines; collapse can enlarge them. Option A correctly contrasts these causes, whereas the other options wrongly assign one agent to both environments.
Which subject and chapter does this question cover?
This is a Class 11 Accountancy question. Chapter: Bank Reconciliation Statement. Topic: Reconciling cash book and passbook differences.
Student feedback
Was this question useful?
👍 0 Helpful 👎 0 Not helpful
Yes 0% No 0%
0 responsesStudent Reviews
No published reviews yet.
