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Intro to Geology Ch 1

Quiz on Notes from 01-15 on Chapter 1

Terms

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Plate Tectonics
Motion and interaction of rigid, interlocking plate-like segments of Earth.
Primary Energy Source
Sun.
Convergent
Two plates collide and one is forced down under the other into the mantle where it is "recycled."This causes quakes and violent volcanic activity.Deep ocean trenches mark where one plate slips under the other.Volcanic island arcs and continental volcanic arcs form next to them.When two continental plates collide, a great mountain range is formed.
Deserts
Very dry climate region.
Dynamic equilibrium
changing balance
Metamorphic
formed when rocks recrystallize without melting, due to heat and pressure deep underground.
Core
Molten outer core, and solid inner core. Iron and nickel composition.
Continental Slopes (below sea level)
Steeper slope that connects shallow sea to deep sea.
Igneous
formed when melted rock (magma) cools and solidifies.
Theory
A hypothesis that has tested true.
Geology
Scientific study of the earth and its major systems.
Geosphere
From the Earth's surface to its center.
Physical Geology
Study of the Earth's composition, structure, and the processes that shape it.
Crust
Outermost and thinnest part of Earth. Two types exist.
Geologic Time
Vast spans of time ranging from thousands to billions of years.
Recycled Materials
the substance of any rock has existed as other rocks in the past.
Stream
Any flowing body of water that is confined to a channel.
Scientific Law
A theory repeatedly tested over many years and never disproved.
Continental
Thicker, variable thickness, and granitic average composition.
Deep Ocean Trenches
Trough-like depressions that are the deepest parts of the oceans.
Primary Water Source
Oceans.
Plateaus
Flat upland region.
The Rock Cycle
Continual transformation of rocks from one type to another.
Lithosphere
Crust + uppermost mantle joined as a single rigid unit. This is what "plates" are made of.
Abyssal Plains
Flat parts of deep ocean.
Sedimentary
formed when rocks weather and erode into sediment that becomes new rock.
Scientific Method
A systematic, logical way of studying how nature works.
Oceanic
Thinner, more uniform in thickness, and basaltic composition.
Hydrosphere
All of Earth's water.
Oceanic Ridges
Undersea mountain range extending through all the oceans.
Plate interaction causes
deformation (bending and breaking).
Transform
Two plates are sliding past one another along a transform fault.There is neither creation nor destruction of lithosphere.Quakes and deformation occur.Features on opposite sides of the boundary are offset.
Continental Shelves (below sea level)
Shallow sea.
Transform Faults
Fractures that cut across a ridge at 90° shifting it right or left.
Divergent plate boundary
Two plates pull apart and move away from one another.As they diverge, magma intrudes into cracks and forms new lithosphere.Almost all occur along the central part (axis) of oceanic ridges.Earthquakes and volcanic activity occur here.
Basins
Flat lowland region.
Atmosphere
Gaseous envelope surrounding Earth.
Mantle
Most of Earth's volume and mass. Denser rock than crust.
The principle of uniformitarianism
Most of Earth's features can be explained by observable processes acting over geologic time spans according to natural laws.
The Hydrologic Cycle
Continuous transfer of water from one repository to another.
Historical Geology
Study of Earth's history and history of life.
Asthenosphere
Highly deformable (plastic) upper mantle.Allows plates to move.
Hypothesis
An attempt to explain the data.
Plains
Flat, gently slope away from mountains.
Volcanic Island Arcs
Curving chains of volcanic islands that are next to a trench.

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