Chapter 11 Weathering, Karst Landscapes, & Mass Movement Flashcards
Physical Weathering
Frost Wedging
Salt-Crystal Growth
Exfoliation
Root Wedging
Factors that influence weathering
- Rock Composition and Structure
- Climate (Precipitation and Temperature)
- Slope Orientation
- Subsurface Water
- Vegetation
Chemical Weathering
Spheroidal Weathering Hydration Hydrolysis Oxidation "Rusting" Dissolution of Carbonates
Solution Sinkhole
Forms due to gradual dissolution of
carbonate rock
- Depths of 7-330 feet; 33-3300 feet wide
Collapse Sinkhole
When a solution sinkhole collapses
through roof of underground cavern
- Develops over hours or days
- Common in Florida
Denudation
Any process that wears away or rearranges landforms
Bedrock
Solid, consolidated rock
Regolith
Rock fragments; broken up
Soil
Rock fragments and finer particles;
dirt; developed from parent material
Physical Weathering:
Frost Wedging
Water penetrates rock through pores (holes) and joints
- When water freezes, it expands; causes wedges in rock to break
Physical Weathering:
Salt-Crystal Growth
Water is easily evaporated in arid regions
- When water evaporates, salt is left behind in pores and joints
Physical Weathering:
Exfoliation
Rock peeling or slipping off in sheets
- Shedding of the outer layer
- Similar to losing outer layers of an onion
Physical Weathering:
Root Wedging
Roots create joints in rock; wedge them apart
Chemical Weathering:
Spheroidal Weathering
Causes the softening and rounding of rock
- Water penetrates rock joints and dissolves or cements weaker minerals
Chemical Weathering:
Hydration
Minerals combining with water
- Structural change; little chemical change