Types of Formations Environmnets
Sedimentary Structures & Environments
Metamorphic Processes & Grades
Name that Rock
Weathering, Minerals & Igneous Features
100

What continuous process describes how rocks transform from one type to another over geological time?

The Rock Cycle

100

This process involves dissolved minerals precipitating out of groundwater to "glue" loose sediments together.

cementation

100

This term refers to the original, unaltered parent rock before it undergoes metamorphism.

protolith

100

Lightweight and filled with gas pockets (vesicles), this extrusive igneous rock can actually float on water.

pumice

100

This surface process breaks down existing surface rocks into smaller sediment pieces through atmospheric exposure, wind, and water.  

weathering

200

Powered by Earth’s internal heat, these rocks form from the cooling and crystallization of molten rock like magma or lava.

Igneous rocks

200

Wavy lines preserved on a rock surface indicate that the rock likely formed in water under the action of waves or currents.

ripple marks

200

This type of localized metamorphism occurs when existing rock is "baked" by adjacent magma intrusions with extreme heat but minimal directional pressure.

contact metamorphism

200

Formed when silica-rich lava cools so rapidly that atoms cannot arrange into a crystalline structure, this rock is also known as volcanic glass.

obsidian

200

According to Bowen's Reaction Series, this highly resistant mineral is the last to crystallize at lower temperatures and forms the primary component of most sandstones.

quartz

300

This primary process describes how loose sediments transform into solid rock through compaction and cementation.

lithification

300

A clastic rock made of large, rounded pebbles requires this level of kinetic energy in its ancient depositional environment to be transported.

a high-energy environment (such as a fast-moving mountain river)

300

Metamorphic rocks that feature a parallel alignment of minerals or a banded appearance due to directional pressure are known by this term.

foliated

300

When limestone is subjected to metamorphic heat and pressure, its calcite crystals recrystallize to form this non-foliated metamorphic rock.

marble

300

Molten rock material deep beneath Earth's surface is called magma, but it receives this name once it reaches or exits Earth's surface.

lava

400

Deep beneath the surface, a large body of magma cooled very slowly over thousands of years, forming large, visible crystals. What rock environment and texture is this?

an intrusive igneous rock with a phaneritic (coarse-grained) texture

400

Because clay particles settle out only in calm, still waters, this fine-grained clastic sedimentary rock forms in low-energy lake beds or deep ocean floors.

shale

400

When a shale protolith undergoes regional metamorphism, state the correct four-step sequence of rocks formed as metamorphic grade increases from low to high.

Slate ---> Phyllite ---> Schist ---> Gneiss

400

Made of the smallest sediment particles (clay) pressed into flat layers, this smooth clastic sedimentary rock easily splits apart.

shale

400

Rapid surface cooling causes extrusive igneous rocks to form this characteristic grain size compared to slow-cooling intrusive rocks.

fine-grained (or microscopic/tiny crystals)

500

In eastern Ohio, compressed carbon-rich ancient plant material that accumulated in stagnant, oxygen-poor swamps formed coal. What specific subtype of sedimentary rock is coal?

an organic sedimentary rock

500

These inclined, crisscrossing sedimentary layers are formed by migrating sand dunes in desert environments or strong water currents.

cross-bedding

500

When sandstone undergoes intense recrystallization, quartz grains interlock into an equant mosaic, forming this non-foliated metamorphic rock.

quartzite

500

Exhibiting a signature silky sheen due to microscopic mica growth, this low-to-medium-grade foliated rock represents the stage between slate and schist.

phyllite

500

During the Silurian period, these sedimentary deposits formed in northeastern Ohio when ancient shallow tropical seas periodically evaporated.

halite (or rock salt) beds

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