EEPS 100 - Module 2: The Lithosphere Flashcards

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Vocabulary flashcards covering the Earth's interior layers, compositional vs mechanical structures, plate tectonics, biogeochemical cycles, rock cycle, and soil horizons from EEPS 100 Module 2.

Last updated 5:08 PM on 9/16/26
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35 Terms

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Goldilocks Zone

The habitable region around a star where physical requirements for life are met, including a suitable temperature range, liquid water, an atmosphere, energy sources, and key elements such as CHNOPS.

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Ionization

The process by which an atom or particle gains or loses electrons, resulting in a charged particle known as an ion.

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Chemical bonding

The joining of two or more atoms together, the strength of which is measured by how much energy is required to break it.

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Compound

A molecule that contains more than one element in its structure.

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Polar molecule

A molecule, such as water, that has an unequal sharing of electrons, resulting in a balance of charges where one side is slightly positive and the other slightly negative.

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Organic molecules

Molecules containing carbon (C\text{C}) atoms bonded to hydrogen (H\text{H}) and other atoms, required for life, including carbohydrates, lipids, proteins, and nucleic acids.

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Energy

The capacity to do work.

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Second Law of Thermodynamics

A physical law stating that entropy (disorder) of an isolated system must increase or stay the same; ecosystems avoid entropy by functioning as open systems that constantly exchange energy and matter with their surroundings.

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Continental Drift

The theory proposed by Alfred Wegener stating that the fit of continental coastlines, along with matching geology, fossils, and mountain belts, indicated past connections between continents.

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Inge Lehmann

The seismologist who discovered that Earth has a solid inner core and a liquid outer core based on observations of seismic shadow zones.

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Inner core

A solid, high-density layer at Earth's center with a radius of approximately 1200km1200\,\text{km}, composed of over 95%95\% iron (Fe\text{Fe}) and around 4%4\% Nitrogen, possessing the highest density and temperature.

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Outer core

A high-density, liquid, hot layer of Earth surrounding the inner core that is approximately 2250km2250\,\text{km} thick.

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Mantle

Earth's layer beneath the crust, approximately 2900km2900\,\text{km} thick, composed of oxygen (O\text{O}), silicon (Si\text{Si}), iron (Fe\text{Fe}), and magnesium (Mg\text{Mg}), which flows like plastic when heated near the outer core.

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Crust

The outermost compositional layer of Earth, ranging from 5100km5\text{--}100\,\text{km} (362mi3\text{--}62\,\text{mi}) thick, which has the lowest density and is cold.

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Lithosphere

The rigid outer mechanical layer of Earth comprised of the crust and upper mantle, which is thicker under continents (10200km10\text{--}200\,\text{km}) and thinner under oceans.

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Asthenosphere

The soft mechanical layer below the lithosphere that can flow over long time periods, whose convective flow provides the energy that moves the lithosphere.

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Earth's magnetic field

A protective shield created by the flow of electrons in molten metal spinning around Earth's solid iron-nickel inner core, protecting the planet from radiation from the sun and space.

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Divergent boundary

A tectonic plate boundary where two plates move away from each other, such as the Mid-Atlantic Ridge.

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Convergent boundary

A tectonic plate boundary where two plates move toward each other, such as the Himalayan mountain range.

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Transform boundary

A tectonic plate boundary where two plates slide horizontally past each other, such as the San Andreas Fault.

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Interior of the Earth

The structural layout of Earth's interior detailing the inner solid core, outer core, lower mantle, upper mantle, oceanic crust, and continental crust.

<p>The structural layout of Earth's interior detailing the inner solid core, outer core, lower mantle, upper mantle, oceanic crust, and continental crust.</p>
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Compositional and Mechanical Layers of Earth

Earth's structural classification divided compositionally into crust, mantle, and core, and mechanically into lithosphere, asthenosphere, mesosphere, outer core, and inner core.

<p>Earth's structural classification divided compositionally into crust, mantle, and core, and mechanically into lithosphere, asthenosphere, mesosphere, outer core, and inner core.</p>
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Rock cycle

The continuous geological process involving weathering, erosion and transport, deposition, burial, deformation and metamorphism, uplift, melting, and solidification.

<p>The continuous geological process involving weathering, erosion and transport, deposition, burial, deformation and metamorphism, uplift, melting, and solidification.</p>
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Weathering

A key process in the rock cycle that breaks down rock materials and makes chemical elements available to other parts of the Earth system.

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Biogeochemical cycle

A cycle in which matter moves through the lithosphere, atmosphere, hydrosphere, and biosphere.

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Pool and Flux

In biogeochemical cycling, a pool is a part of an ecosystem where matter resides, while flux is the rate at which matter moves between pools.

<p>In biogeochemical cycling, a pool is a part of an ecosystem where matter resides, while flux is the rate at which matter moves between pools.</p>
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Igneous rocks

Rocks formed through crystallization from magma or lava.

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Sedimentary rocks

Rocks formed from sediments that are deposited, buried, and cemented together via lithification.

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Metamorphic rocks

Rocks that have undergone structural or mineralogical changes due to heat and pressure.

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Mineral

A naturally occurring solid with a defined internal arrangement of atoms that serves as the natural building block of rocks.

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Calorie

The unit representing the amount of energy required to raise the temperature of 1g1\,\text{g} of water by 1C1\,^{\circ}\text{C}.

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Gyres

Circular current patterns found in major oceans.

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Zone of leaching (E horizon)

The soil layer where dissolved or suspended materials are carried downward by water.

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Zone of accumulation (B horizon)

The soil layer where iron, aluminum, and clay leached down from the E horizon accumulate, containing soluble minerals like calcite in drier climates.

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Soil Profile

The vertical succession of soil horizons, including O (organic matter), A (organic matter mixed with rock/mineral fragments), E (zone of leaching), B (zone of accumulation), C (weathered parent material), and Bedrock.

<p>The vertical succession of soil horizons, including O (organic matter), A (organic matter mixed with rock/mineral fragments), E (zone of leaching), B (zone of accumulation), C (weathered parent material), and Bedrock.</p>