Lesson 1 Physical and Chemical Weathering
Jekyll Island Overview
Location: Off the coast of Georgia, Glynn County.
Ownership: Owned by the State of Georgia, self-governing body.
Attractions: Popular tourist destination with beaches, bike trails, Summer Waves water park.
Historic District: Features buildings from the late 19th and early 20th centuries.
Wildlife: Home to various mammals, reptiles, and birds in salt marshes.
Weathering
Definition: Breaking down or dissolving of rocks and minerals on Earth's surface.
Types:
Physical Weathering
Chemical Weathering
Physical Weathering
Involves mechanical breakdown without changing chemical composition.
Causes:
Wind
Water
Effects: Rocks become smaller, rounded, lose sharp edges. Can cause holes due to abrasion.
Unique Process: Freezing and thawing of water causes expansion, leading to rock fracturing.
Example of Physical Weathering
Scenario: Statues at a library rounded and less detailed due to weathering.
Cause: Likely weathering of the stone.
Chemical Weathering
Definition: Breakdown of rock through chemical reactions.
Examples:
Reaction with water (e.g., Alka Seltzer in water forming carbonic acid).
Iron rusting due to oxidation.
Significance: Forms new substances, important in cave and sinkhole formation.
Erosion and Deposition
Erosion: Movement/transportation of rock materials, caused by gravity or weather.
Deposition: Dropping off of eroded materials in new locations, forms features like river deltas.
Importance: Changes Earth's surface significantly over time; affects landforms like the Grand Canyon.
Groundwater and Aquifers
Definition: Fresh water in openings of soil and rock, crucial for drinking water supply.
Aquifers: Porous rock/soil formations that can store groundwater (e.g., limestone, gravel).
Acids in Weathering
Role of Acids: Acids formed during rock alteration or from rain dissolve minerals.
Common Acid: Carbonic acid through CO2 and water reaction.
Consequences: Vital in sinkhole formation.