Earth Science

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Last updated 4:16 AM on 6/5/26
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17 Terms

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Geosphere

Solid Earth, including rocks, minerals, soil, Earth’s core, & landforms that make up the planets crust

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Hydrosphere

All the liquid water on and beneath the surface of the Earth (oceans, lakes, groundwater, etc)

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Cyrosphere

frozen water (glaciers, ice gaps, sea ice)

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Atmosphere

The thin layers of gases (Nitrogen & Oxygen) that surrounds the planet, regulating weather & climate

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Biosphere

All living organisms on Earth (Plants, animals, & humans)

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Patterns in ages

Possible answers - Increases in one direction across map OR rocks get older as you move farther away from mid ocean ridge

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Compass direction

Possible answers - Plate is moving in the direction of the older rocks OR The feature moved towards the older ages or away

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Zircon

  • Usually found In Igneous rocks

  • Hard

  • Resistant to weathering

  • Incorporates Uranium (measure to determine age)

  • Slowly decays into lead

  • Radiometric dating

  • Used to determine age of rocks

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Cross - cutting Relationships

Any feature that cuts across a rock layer must be younger than the rock it cuts through

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Ice Sheets vs. Ocean Levels

When Earth cools and massive glaciers form, global sea levels drop —— When glaciers melt, sea levels rise, flooding coastal regions

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Plate tectonics

Theory that Earth’s rigid outer shell (Lithosphere) is broken into several, massive, moving slabs

Convection Currents - Magma in mantle acting as a slow moving conveyor belt that pushes and pulls the overlying plates

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3 Types of Plate Boundaries

Convergent - crashing

Divergent - separating

Transform - sliding

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Continental drift & Fossil Evidence

  • Continents once joined together

  • Formed a single landmass (pangaea)

  • Plate tectonics split & drifts continents apart of MYA

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Subsidence

Sinking of the Earth’s surface

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Uplift

Rising of Earth’s crust causing weathering & erosion

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Correlation

Matching rock layers across different locations based on index fossils or rock characteristics

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Half - Lives

The time it takes for half of the radioactive atoms In a sample to decay into a stable product