complex mountains
mountain building
national parks
complex geology
geological features
100

this state is home to grand teton national park

wyoming

100

The first stage of major mountain belt building involves the deposition of thick layers of sedimentary or volcanic rock, known as this stage.

the accumulation stage

100

 Located in eastern Nevada, this park is known for its remote location and Basin and Range topography.

Great Basin National Park

100

The oldest rocks exposed in the Grand Teton mountains are from this geologic eon.

the Precambrian

100

This term describes fractures or cracks in the Earth's surface where there is no significant displacement.

joints

200

the active mountain building stage in the formation of major mountain belts is known as this

the orogenic stage

200

After the active mountain-building stage, this process often occurs due to isostatic rebound.

crustal extension and uplift

200

Unlike the broad, rounded mountains of the Appalachian Mountains (Module 5), the Tetons are characterized by their sharp peaks and lack of these.

foothills

200

Great Basin National Park is located within this physiographic province characterized by alternating mountain ranges and valleys formed by normal faulting.

 the Basin and Range

200

 The Grand Teton peak itself is an example of this sharp, pyramid-shaped mountain formed by the erosion of multiple glacial cirques.

horn

300

The stable, interior portion of a continent, often containing the oldest rocks, is called this. 

the craton

300

The process by which a continent gains land on its tectonically active margins, often through subduction or continental collision, is called this.

tectonic accretion

300

This Arkansas national park, while located in a complex geological area, is primarily known for its geothermal features rather than dramatic block faulting.

hot springs national park

300

A downward fold in rock layers, where the youngest rocks are typically found in the center, is called this.

syncline

300

This type of fault occurs when tensional forces pull rocks apart, causing the hanging wall to move down relative to the footwall.

normal fault

400

This type of crustal deformation involves the bending of rock layers.

folding

400

An upward fold in rock layers, where the oldest rocks are typically found in the center, is called this.

anticline 

400

This California national park, discussed in a previous module, is known for its arches and hoodoos, formed by weathering along joints.

Arches National Park or Bryce Canyon National Park

400

These fractures or cracks in the Earth's surface involve displacement or movement caused by tectonic forces.

faults

400

The steep, knife-edged ridges that separate adjacent glacial valleys in the Tetons are called these.

aretes

500

Grand Teton National Park's dramatic scenery is primarily a result of this type of faulting.

normal faulting (block faulting)

500

This national park in Utah features a prominent monocline known as the Waterpocket Fold.

capitol reef national park

500

 Both Grand Teton National Park and this Maine national park (mentioned in the context of tectonic accretion in Module 6) owe some of their protected land to donations from John D. Rockefeller.

 Acadia National Park

500

The metamorphic core complexes found in many of the mountain ranges within the Basin and Range province are primarily composed of these types of rocks.

crystalline rocks (schist and gneiss)

500

The thinning and extension of the continental crust in the Great Basin region during the Cenozoic led to the formation of these types of faults.

normal faults