River Valley Profiles: Unveiling the Characteristics and Processes of Waterways

River Valley Profiles: Unveiling the Characteristics and Processes of Waterways

Assessment

Interactive Video

Science, Geography, Biology

6th - 8th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video tutorial by Andy explores the three sections of a river: upper, middle, and lower courses. Each section has distinct characteristics and processes. The upper course is steep and mountainous, with fast-flowing water causing significant erosion, forming features like waterfalls and gorges. The middle course is flatter, with slower water flow, leading to transportation and the formation of meanders and oxbow lakes. The lower course is extremely flat, where deposition is the main process, creating features like river deltas and floodplains. The video emphasizes the importance of these features to wildlife and ecosystems.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What are the three main sections of a river?

Source, Middle, End

Upper, Middle, Lower

High, Medium, Low

Start, Center, Finish

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the main process occurring in the upper course of a river?

Transportation

Erosion

Deposition

Sedimentation

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which feature is commonly formed in the upper course of a river?

Oxbow Lake

Floodplain

Waterfall

Delta

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What shape are the valleys typically found in the middle course of a river?

Circular

Flat

U-shaped

V-shaped

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the main process occurring in the middle course of a river?

Erosion

Evaporation

Transportation

Deposition

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What feature can develop from meanders in the middle course?

Gorge

Waterfall

Delta

Oxbow Lake

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Where does a river typically meet the sea?

Middle Course

Lower Course

Upper Course

Source

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