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What is a natural hazard?
A normal Earth process that becomes hazardous when humans are exposed to it.
Can most natural hazards be eliminated?
No. Most are beyond human control.
Why should we anticipate disasters?
To save lives and money.
What can turn a hazard into a disaster?
Human exposure to the hazard.
What can turn disasters into catastrophes?
Social factors and increased impacts.
What is risk?
Probability × Potential Impact.
What does mitigation mean?
Reducing the effects of a hazard.
Responding after an event happens.
Search and rescue.
Firefighting.
Reducing vulnerability before an event.
Enforcing building codes.
It can greatly reduce loss of life and property.
Regulating land use to create better social and environmental outcomes.
Science helps predict hazards; risk helps decisions; hazards are linked; humans can worsen disasters; impacts can be minimized.
Heat from Earth's interior and Earth's gravity.
Earthquakes, volcanoes, and landslides.
Energy from the Sun and objects from space.
Weather, storms, drought, wildfires, flooding, and impact events.
Human actions that alter natural systems.
Climate change, fires, or erosion.
Processes that create, maintain, modify, and recycle Earth's surface materials.
Tectonic, rock, hydrologic, and biogeochemical cycles.
The creation, movement, and destruction of tectonic plates.
Ocean basins, mountain belts, and volcanic chains.
Earthquakes and volcanoes.
A natural inorganic solid with defined chemistry and crystalline structure.
An aggregate of one or more minerals.
Igneous, sedimentary, and metamorphic.
The continuous movement of water through Earth systems.
Evaporation, precipitation, and runoff.
The Sun and gravity.
A place where water is stored.
The average time water stays in a reservoir.
Cycles that move essential elements through Earth's systems.
Carbon, oxygen, nitrogen, and phosphorus.
A benefit that a natural hazardous process provides to the environment or humans.
They can create new land.
They can help capture resources.
They can distribute nutrients.
Crust, mantle, and core.
Rock.
Oxygen, silicon, and aluminum.
It is the least dense major chemical layer.
About 7–75 km.
Rock containing oxygen, silicon, magnesium, and iron.
About 2,900 km.
Mostly iron and nickel.
Very dense.
About 3,500 km.
The separation of materials based on density.
They sink.
They rise.
It sank toward the core.
They rose toward the surface.
Lithosphere, asthenosphere/upper mantle, lower mantle, outer core, and inner core.
A rigid, strong layer containing the crust and uppermost mantle.
Tectonic plates.
A weak, plastic layer that can flow over time.
The asthenosphere.
A solid layer about 2,300 km thick.
A liquid layer.
A solid layer.
Thick, less-dense crust.
About 30–50 km.
Thin, denser crust.
How thick is oceanic crust?
About 6–7 km.
Which is denser: oceanic or continental crust?
Oceanic crust.
What is plate tectonics?
The theory that Earth's lithosphere is divided into moving plates.
What can plate movement cause?
Earthquakes, volcanoes, and mountains.
The idea that continents move over geologic time.
Alfred Wegener.
German meteorologist.
1912.
It was widely rejected.
A supercontinent containing most of Earth's continental blocks.
About 330 million years ago.
About 200 million years ago.
"All the earth."
The ancient climate of an area.
That continents were once connected.
The same species are found on continents now far apart.
The study of underwater depth of ocean floors.
Mid-ocean ridges.
New oceanic crust forms at mid-ocean ridges and moves away.
Near mid-ocean ridges.
Farther away from mid-ocean ridges.
The direction and amount of plate movement.
About 5 cm per year.
Transform, divergent, and convergent.
Two plates slide past each other.
The San Andreas Fault.
Strong to major earthquakes.
No.
Two plates pull apart.
It rises and forms new crust and lithosphere.
The Mid-Atlantic Ridge/Iceland.
Two plates move toward each other.
The denser oceanic plate subducts beneath the continental plate.
Strike-slip, normal, and reverse.