Unit 1 - Page 5 - 8

Unit 1 - Page 5 - 8

11th Grade

20 Qs

quiz-placeholder

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Unit 1 - Page 5 - 8

Unit 1 - Page 5 - 8

Assessment

Quiz

Geography

11th Grade

Medium

Created by

J Martin

Used 3+ times

FREE Resource

20 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

What does a storm hydrograph show?

The annual variation in river discharge

The daily variation in river discharge

The response of a river’s discharge to a rainfall event

The long-term impact of human activity on rivers

Answer explanation

Answer: c) The response of a river’s discharge to a rainfall event

  • Explanation: A storm hydrograph tracks how much water flows in a river after it rains. For example, if it rains heavily in a city, the hydrograph will show how quickly the water reaches the river and how much the flow increases.

2.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

What is the main contributor to river discharge before a storm?

Quickflow

Groundwater flow/baseflow

Overland flow

Channel precipitation

Answer explanation

Answer: b) Groundwater flow/baseflow

  • Explanation: Before it rains, rivers get their water mainly from groundwater slowly seeping into the riverbed. Imagine a river in a dry season—it's still flowing because of underground water sources.

3.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

During a storm, what type of flow occurs when water runs over the surface directly into a river?

Quickflow

Throughflow

Baseflow

Rising limb

Answer explanation

Answer: a) Quickflow

  • Explanation: When it rains heavily, some water can’t soak into the ground, so it flows over the surface straight into rivers. Think of rain on a paved road; water quickly moves into storm drains and nearby rivers.

4.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

What does the rising limb of a storm hydrograph represent?

The decline in river discharge after the storm

The speed at which water infiltrates the soil

The increase in river discharge during a storm

The time taken for rainfall to reach the river

Answer explanation

Answer: c) The increase in river discharge during a storm

  • Explanation: This part of the graph shows how fast the river's water level rises after it starts raining. For instance, during a flash flood, the rising limb is very steep because water flows into the river quickly.

5.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

What is the recessional limb of a storm hydrograph?

The peak discharge of the river

The decrease in river discharge after the storm

The total volume of water in the river

The time between the storm start and peak flow

Answer explanation

Answer: b) The decrease in river discharge after the storm

  • Explanation: After the rain stops, the river's water level slowly drops. This part of the graph shows the time it takes for the river to return to normal levels. Imagine a river slowly calming down after a flood.

6.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

What does the peak flow on a storm hydrograph indicate?

The maximum rainfall during a storm

The maximum discharge of the river during a storm

The time it takes for the river to return to baseflow

The average discharge of the river over time

Answer explanation

Answer: b) The maximum discharge of the river during a storm

  • Explanation: This is the highest point on the graph and shows the maximum amount of water flowing in the river. During a flood, the peak flow is when the river is at its fullest.

7.

MULTIPLE CHOICE QUESTION

15 mins • 1 pt

What is the time lag on a storm hydrograph?

The time between the start of the storm and peak rainfall

The time between peak rainfall and peak discharge

The time between the end of the storm and baseflow

The time between the rising limb and recessional limb

Answer explanation

Answer: b) The time between peak rainfall and peak discharge

  • Explanation: Time lag shows how long it takes for rain to reach the river. In cities with lots of concrete, the time lag is short because water moves fast. In forests, the time lag is longer because trees and soil absorb water first.

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