Geological Hazards and Natural Disasters

Geological Hazards and Natural Disasters

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@GallantBinary

Questions and Answers

What type of rocks are commonly found in karst terrains where sinkholes develop?

Limestone, dolomite, or gypsum

What is the primary factor responsible for the formation of sinkholes?

Groundwater dissolving bedrock

Which of the following is NOT a type of geological hazard discussed in the chapter?

Earthquakes

What is the purpose of monitoring warning signs of geological hazards?

<p>To prepare for and mitigate the impacts of the hazard</p> Signup and view all the answers

What is the concern related to near-earth objects mentioned in the chapter?

<p>Their potential to collide with Earth</p> Signup and view all the answers

What is the primary mechanism underlying the formation of dissolution sinkholes?

<p>Dissolution of limestone or dolomite by water or acid</p> Signup and view all the answers

What is the primary factor that contributes to the formation of cover-subidence sinkholes?

<p>Permeability of covering sediments containing sand</p> Signup and view all the answers

Which of the following signs is NOT indicative of an impending landslide?

<p>Increased gravity readings</p> Signup and view all the answers

What is the potential consequence of a bolide impact on Earth's environment?

<p>Sea level changes and tectonic activities</p> Signup and view all the answers

What is the primary cause of slope saturation leading to landslides?

<p>Torrential rainfall</p> Signup and view all the answers

Study Notes

Natural Hazards

  • Sinkholes develop in areas with karst terrains, which have bedrocks made of limestone, dolomite, or gypsum that can be dissolved by groundwater over time.
  • Formation of sinkholes is often a result of the dissolution of these rocks, leading to the creation of underground spaces or caverns.
  • There are four types of sinkholes: dissolution, cover-subsidence, human-induced, and cover-collapse sinkholes.

Types of Sinkholes

  • Dissolution Sinkholes: form from the dissolution of limestone or dolomite by water or acid, often intensifying where water first contacts the rock surface or through pre-existing openings.
  • Cover-Subsidence Sinkholes: develop in areas where covering sediments are permeable, containing sand.
  • Human-Induced Sinkholes: associated with human activities like groundwater pumping, construction, and land development practices.
  • Cover-Collapse Sinkholes: occur where covering sediments contain a significant amount of clay, leading to abrupt development and potential catastrophic damages.

Landslides

  • Heavy rainfall can contribute to landslides in several ways: slope saturation, loosening of soil, and disturbance to terrain.
  • Signs of an impending landslide include:
    • Physical changes: cracks or bulges on concrete or paved roads, sidewalks, and structures.
    • Broken underground fixtures: indicating potential ground movement.
    • Changes in land: sudden changes in the landscape, such as tilting trees or leaning utility poles.
    • Unusual sounds: sounds like cracking or rumbling coming from the ground.
    • Sediments in water: increased turbidity in nearby water bodies due to soil erosion.
    • Slope movement: visible movement or slumping of soil or rocks on slopes.

Near-Earth Objects (NEOs)

  • NEOs pose various potential impacts on Earth, including:
    • Direct Impact: NEOs like asteroids or comets colliding with Earth can cause significant damage, leading to loss of life, destruction of property, and environmental consequences.
    • Climate Change: bolide impacts can result in climate change, sea level changes, tectonic activities, earthquakes, and increased volcanism, affecting global ecosystems and potentially leading to mass extinctions.
    • Geological and Environmental Impacts: NEO impacts can affect geological, geophysical, and environmental systems.

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