Folds & Faults
Stages & Ages
Cores, Fractures & Rocks
Types of Faults
Parks
100

A type of fold is where rocks are folded upward in an arch

Anticline Fold

100

Great thicknesses of sedimentary rocks and/or volcanic rocks are deposited

Accumulation Stage

100

Biologic sedimentary rock that formed from the accumulation of billions of tiny plankton skeletons made of silica

Chert

100

The actual surface of the fault

Fault Plane


100

Most visited National Park

Great Smoky Mountains National Park

200

A type of fold where rocks are folded downward in a trough pattern

Syncline Fold

200

The mountain-building stage which begins while accumulation occurs, causes folding and faulting

Orogenic Stage

200

Fractures or cracks in the earth’s surface at which there is no displacement

Joints

200

The rock directly above the fault

Hanging Well

200

Very popular location for filming movies in the desert due to its proximity to Hollywood

Joshua Tree National Park

300

The breaking displacement of rock

Faults

300

The addition of exotic terranes to a continental land mass which is usually caused by intense plate collisions

Tectonic Accretion

300

A slightly metamorphosed chert with cryptocrystalline structure

Novaculite

300

The rock directly below the fault

Footwall

300

Hottest and driest place in the United States

Death Valley National Park

400

These are most common faults at transform boundaries such as those found at the bottom of the ocean, or on land

Strike-slip Faulting

400

The stable, interior portion of continent, usually very old crystalline rocks. The oldest rocks in the world are found here

Craton

400

The core of low-grade Precambrian and Paleozoic rocks faulted over each other, and there is extensive metamorphism, folding, and low-angle faulting

Metamorphic Core Complex

400

Tensional, or extensional, forces pull the rocks apart, create a fault, and the hanging wall falls down relative to the footwall

Normal Faulting


400

Home to the tallest tree in the world

Redwood National Park

500

Trace of the fault on the land surface or where you can see the fault

Fault Scarp


500

Occurs during isostatic rebound of crustal plates, after orogenic stage, surface weathering and erosion occurs during this stage

Crustal Extension, Block Faulting, and Uplift Stage

500

A mixture of diverse materials scraped off the top of the subducting oceanic plate

Mélange

500

Compressional forces push the rocks together, creating a fault, and the hanging wall is pushed up relative to the footwall

Reverse & Thrusting Fault

500

Smallest national park

Hot Springs National Park

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