Geology of the Uinta Mountains

Geology of the Uinta Mountains

Assessment

Interactive Video

Geography

9th - 10th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video explores the unique east-west orientation of the Uinta Mountains in northeastern Utah, contrasting with the typical north-south trend of other western US mountain ranges. It delves into the geologic history, from the Precambrian era to the formation of the supercontinent Rodinia, and the development of rift basins. The video examines field evidence of sedimentation and depositional environments, highlighting the role of braided streams. It concludes with the Laramide Orogeny, which uplifted the Uinta Mountains, exposing the Uinta Mountain Group.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the unique orientation of the Uinta Mountains compared to most other mountain ranges in the western US?

Northeast-Southwest

North-South

East-West

Southeast-Northwest

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which peak is the tallest in Utah, located in the Uinta Mountains?

Mount Nebo

Mount Timpanogos

Kings Peak

Deseret Peak

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

During which period did the last glacial maximum occur in the Uinta Mountains?

25,000 years ago

10,000 years ago

15,000 years ago

20,000 years ago

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What significant geological event occurred around 1 billion years ago?

Formation of the Rocky Mountains

Assembly of the supercontinent Rodinia

Formation of the Atlantic Ocean

Breakup of Pangaea

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What type of faults formed the rift basins in the Uinta Mountains?

Strike-slip faults

Thrust faults

Reverse faults

Normal faults

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What type of sedimentary rocks are primarily found in the Uinta Mountain Group?

Limestone

Basalt

Granite

Coarse-grained sandstone

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What geological process led to the uplift of the Uinta Mountains during the Laramide orogeny?

Sea level rise

Compression from a subduction zone

Erosion

Volcanic activity

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