Science Test: Rocks and Earth Structure

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Comprehensive vocabulary flashcards covering Earth layers, tectonic plate boundaries, rock types (sedimentary, metamorphic, igneous), weathering mechanisms, the rock cycle, fossil formation, and specific rock specimens.

34 Terms

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Crust

The solid outermost layer of the Earth, extending from 0–100 km0\text{--}100\,\text{km} in depth.

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Mantle

The semi-liquid layer of the Earth located between 100 km100\,\text{km} and 2900 km2900\,\text{km} beneath the crust.

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Outer Core

The liquid layer of the Earth's interior situated between 2900 km2900\,\text{km} and 5100 km5100\,\text{km} in depth.

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Inner Core

The solid central layer of the Earth extending from 5100 km5100\,\text{km} to 6378 km6378\,\text{km}.

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Divergent Plate Boundary

A plate boundary where tectonic plates move apart from each other, creating landforms such as volcanoes, valleys, and canyons (e.g., Red Sea formation).

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Transform Plate Boundary

A plate boundary where tectonic plates slide horizontally past one another, forming faults and causing earthquakes (e.g., Alpine Fault).

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Convergent Plate Boundary

A plate boundary where tectonic plates collide or move toward one another, forming landforms such as volcanoes and mountains (e.g., Himalayas, The Alps).

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Weathering (Rock Cycle)

The initial geological process of breaking rocks down into small pieces.

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Erosion

The process by which rock sediments are carried away by water and wind.

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Deposition

The stage in sedimentary rock formation where transported sediments are dropped on top of each other.

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Compaction

The process in which accumulated sediment layers are pressed tightly together by overlying weight.

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Cementation

The process in which dissolved minerals act as glue to bind compacted sediment particles together.

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Sedimentary Rock

A category of rock formed through weathering, erosion, deposition, compaction, and cementation; characterized by layers, a grainy texture, a softer structure, and the potential presence of fossils (e.g., sandstone, chalk, limestone, shale, mudstone, coal).

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Metamorphic Rock

A rock formed deep underground when an existing parent rock changes due to extreme heat and pressure; characterized as hard, dense, devoid of fossils, and potentially showing foliation or crystals (e.g., quartzite, slate, marble, gneiss, schist).

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Foliation

Layering or banding observed in certain metamorphic rocks as a result of directed pressure.

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Igneous Rock

A rock formed when molten lava or magma cools and crystallizes; typically hard, non-layered, often crystalline, and capable of displaying a glassy texture or vesicles.

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Intrusive Igneous Rock

An igneous rock that cools slowly beneath the Earth's surface, allowing the growth of large crystals (e.g., granite).

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Extrusive Igneous Rock

An igneous rock that cools rapidly on the Earth's surface, resulting in the formation of small crystals (e.g., basalt).

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Vesicles

Small cavities or holes present in volcanic igneous rocks, formed by trapped gas bubbles during cooling.

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Physical Weathering

A mechanical breakdown process that fractures rocks into smaller fragments without altering their chemical composition, akin to cracking or smashing a rock.

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Freeze-Thaw

A mechanism of physical weathering in which water enters cracks in a rock, freezes, expands, and consequently widens the crack.

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Chemical Weathering

The breakdown and alteration of a rock's internal minerals via chemical reactions, which causes the rock to soften, dissolve, or transform into new substances.

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Acid Rain Weathering

A form of chemical weathering where rainwater containing dissolved carbon dioxide dissolves susceptible rocks such as limestone.

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Biological Weathering

The disintegration of rocks caused by the activities of plants, animals, and microorganisms, such as plant roots wedging cracks apart or burrowing animals digging into rock crevices.

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Limestone Weathering Equation

CaCO3+H2SO4→CaSO4+H2O+CO2CaCO_3 + H_2SO_4 \rightarrow CaSO_4 + H_2O + CO_2, representing the reaction of calcium carbonate with sulfuric acid to yield calcium sulphate, water, and carbon dioxide.

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Silica (in Fossilization)

The mineral compound that gradually replaces calcium phosphate in an organism's bones during the fossilization process.

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Trace Fossils

A classification of fossils that record geological evidence of biological activity (such as footprints or burrows) rather than anatomical remains.

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Mold Fossils

A type of fossil formed when an organism decays within sediment, leaving an impression or negative space of its shape in the surrounding rock.

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Resin Fossils

Fossils formed when organisms are trapped and preserved inside ancient hardened tree sap or amber.

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Body Fossils

Fossils consisting of preserved actual physical structures or skeletal remains of an organism.

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Granite

A hard, intrusive igneous rock characterized by large crystalline grains.

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Schist

A medium-grained metamorphic rock whose original precursor or parent rock is a protolith.

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Sandstone

A grainy sedimentary rock composed of numerous accumulated layers of mineral or rock sediment.

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Marble

A crystalline metamorphic rock produced when its parent rock, limestone, is subjected to heat and pressure.