Peru: Weathering, Erosion, and Landforms
Weathering and Mass Wasting
Peru experiences both chemical and physical weathering due to its diverse geography.
- Carbonation: Rainwater dissolves limestone in mountainous areas.
- Hydrolysis: Breaks down minerals in humid regions like the Amazon.
- Freeze-thaw: Cracks rocks in the Andes Mountains.
Mass wasting (landslides) occurs frequently because of steep slopes, heavy rainfall, and earthquakes.
Major Event: In 1970, an earthquake triggered an avalanche from Mount Huascarán, burying the town of Yungay and killing ~20,000 people.
Government Response:
- Early warning systems
- Landslide monitoring
- Building restrictions
- Emergency planning
Water Erosion
Major Rivers
- Amazon River: Source in Andes, ~6,400 km long, largest discharge in the world, meandering channel.
- Ucayali River: Braided/meandering, major Amazon tributary.
- Marañón River: Flows through canyons, used for hydroelectric power.
Impacts
- Loss of farmland
- Flooding
- Damage to infrastructure
- Displacement of communities
Government Solutions
- Levees and flood barriers
- Riverbank stabilization
- Reforestation
- Flood monitoring
Wind Erosion
Wind erosion mainly occurs along Peru’s coastal deserts.
- Sand dunes form from strong coastal winds
- Common in Nazca and Paracas regions
Government Actions:
- Planting vegetation to stabilize sand
- Protecting desert areas
Deserts and Desertification
Major Deserts
- Sechura Desert: Reg (gravel desert), largest in Peru
- Nazca Desert: Reg + hamada (rocky desert), home of Nazca Lines
Desertification Issues:
- Climate change
- Overgrazing
- Deforestation
Government Solutions:
- Reforestation
- Sustainable farming
- Water conservation
Glaciers
Peru has the largest number of tropical glaciers, mainly in the Andes (Cordillera Blanca).
Importance
- Water supply
- Agriculture
- Hydropower
Problems
- Glacier melting due to climate change
- Water shortages
- Flood risks from glacial lakes
Glacial Features
- U-shaped valleys
- Glacial lakes
- Moraines