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How does a lapies or clint-and-grike surface form?

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Answer and explanation

Correct answer: By solution widening cracks on a limestone surface

Lapies, also called clints and grikes, are characteristic karst features on exposed limestone. Rainwater, made slightly acidic by dissolved carbon dioxide, enters joints and chemically dissolves the limestone. Continued solution widens and deepens the cracks, leaving blocks or clints separated by grooves called grikes. Thus option C is correct; the other choices describe glacial, coastal, or fluvial deposition rather than limestone solution.

Related tags

LapiesClint And GrikeKarst SolutionLimestone WeatheringRecording Of Transactions (I & Ii)Recording Of Transactions I IiAccountancyClass 11 Mcq

Frequently asked questions

What is the correct answer to this question?

By solution widening cracks on a limestone surface

Why is this the correct answer?

Lapies, also called clints and grikes, are characteristic karst features on exposed limestone. Rainwater, made slightly acidic by dissolved carbon dioxide, enters joints and chemically dissolves the limestone. Continued solution widens and deepens the cracks, leaving blocks or clints separated by grooves called grikes. Thus option C is correct; the other choices describe glacial, coastal, or fluvial deposition rather than limestone solution.

Which subject and chapter does this question cover?

This is a Class 11 Accountancy question. Chapter: Recording of Transactions (I & II).

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