ThinkRankLandforms and their Evolution
Landscape evolution is the result of erosional and depositional work by agents like water, wind, and ice. This chapter examines the specific landforms created by rivers, glaciers, groundwater, and more.
Learning Objectives
- •Identify fluvial, glacial, and aeolian landforms
- •Explain the cycle of erosion and landform maturity
- •Describe the unique features of Karst topography
- •Analyze the role of waves in coastal geomorphology
Key Concepts
Landscape Maturity
Landforms pass through youth, maturity, and old age stages. For example, a river in its youth carves deep V-shaped valleys, while in old age, it meanders through broad plains.
Karst Topography
Found in limestone regions, where groundwater dissolves rock to form caves, sinkholes, stalactites, and stalagmites.
Terminology
Historical Insight
Mississippi Delta
A classic example of a river's depositional landform at the end of its life cycle.
Quick Check
What is a Cirque?
How is an Ox-bow lake formed?
How to use this lesson
Read the overview first, then explain the main idea in your own words before checking the key concepts. Use the quick-check questions without looking at the answer. For examination preparation, verify dates, definitions, and syllabus requirements against your official textbook and school or examination-board guidance.
Test Your Knowledge
Ready to check your understanding of this chapter? Take our interactive practice quiz.