GEOG- Exam 3 Flashcards
Frostwedging
Mechanical Weathering- Water gets into cracks in rocks & freezing enlarges the cracks
Salt Crystal Growth Process:
- sea spray to salty groundwater gets in rock cracks
- salt crystals form and when water evaporates it enlarges the cracks
- rocks eventually crack
Sheeting Process:
Pluton (intrusive igneous rock landforms) exposed after erosion removes younger rock that covered it
Rock slabs break due to release of confining pressure (weight of material above causing pressure from all sides)
Exfoliation dome forms after enough time passes *associated with pluton and weight of material pushing down on it
*Example: Half dome in Yosemite
bio activity with mechanical
plant roots
Karst Topography
Karst topography is a type of landscape that forms from the dissolution of soluble rocks, such as:
-Limestone
-Dolomite
-Gypsum
Key Features of Karst Topography:
Sinkholes – Depressions or holes in the ground caused by collapse of a surface layer.
Caves and Caverns – Formed as acidic water dissolves rock underground.
Disappearing streams – Rivers or streams that vanish into the ground.
Springs – Where underground water emerges at the surface.
🧪 How It Forms:
Rainwater absorbs carbon dioxide from the atmosphere and soil, becoming slightly acidic.
This weak acid reacts with the carbonate in rocks like limestone.
Over time, water slowly dissolves the rock, creating underground voids and surface features.
Karst areas are important for groundwater storage, but they can also be risky for construction due to sudden sinkhole formation.
-calcium carbonate and underground dissolving
Weathering
physical breakdown &/or chemical alteration of rock at or near Earth’s surface
Erosion
removal & transport of weathered rock by water, wind, or ice
Differences between weathering and erosion:
Weathering breaks down rocks and minerals in place, while erosion transports the broken-down materials away from their original location.
Mechanical Weathering
Physical forces breaking rocks into smaller pieces
Chemical Weathering
Chemical weathering is the process by which rocks and minerals break down due to chemical reactions, often involving water, acids, and gases. Unlike physical weathering, which just breaks rocks apart, chemical weathering changes the actual composition of the rock.
How do mechanical & chemical weathering work together?
Mechanical increases surface area, speeding up chemical reactions.
Karst valleys –
Created as sinkholes merge or expand over time.
Examples of mechanical weathering?
Frost wedging (ice expands in cracks), abrasion (rocks grind), root wedging, salt crystal growth.
What is sheeting?
Expansion and cracking of rock as overburden is removed. Creates exfoliation domes with onion-like layers.
Examples of chemical weathering?
Hydrolysis (water + minerals), oxidation (rust), carbonation (acid dissolves limestone), dissolution (minerals dissolve in water).
What is a solvent?
A liquid that dissolves other substances.
What is a homogeneous solution?
A mixture where the components are evenly distributed.
Two main factors influencing weathering rate?
Climate (especially moisture & temperature), and rock type (mineral composition/solubility)
What is solubility?
A substance’s ability to dissolve in a solvent.
What is regolith?
A layer of loose rock and mineral fragments covering bedrock.
What is soil?
A mixture of mineral particles, organic material, air, and water.
What is humus?
Decayed organic matter in soil.
What is loam?
Soil with a balanced mix of sand, silt, and clay.
3 soil particles ranked by size?
Sand (largest)
silt
clay (smallest)