Lesson Y8-U01-L08
Y8-U01-L08 Living with Earthquakes: Japan and Tōhoku, 2011 Quiz: KS3 Geography, Unit 7
20 questions
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Lesson Y8-U01-L08, Living with Earthquakes: Japan and Tōhoku, 2011: 20 multiple choice questions for the KS3 Geography (National Curriculum), Unit 7: Year 8: Restless Earth: Tectonic Hazards, written with Revision Ninja.
Host it live on the board and students join with a game code on their own devices, or revise alone with Free Play. The answers are revealed in the game.
The 20 questions
-
What is a tsunami?
- A fast-flowing river that floods nearby towns after heavy rain in the mountains
- A strong wind that blows across the sea and raises waves
- A giant wave of mud that flows down a volcano's slopes
- A huge sea wave set off by an undersea earthquake or eruption
-
What does HIC stand for in this lesson?
- High-Income Country
- High-Impact Crisis
- Horizontal Infrastructure Clearance
- Hazard Index Count
-
What is the Pacific Ring of Fire?
- A ring of coral reefs that surrounds the Pacific islands
- A line of high mountains across the centre of Asia
- A cluster of hot springs in the Atlantic Ocean, found around the islands of the Caribbean
- A zone of many earthquakes and volcanoes around the Pacific Ocean
-
Which large ocean lies to the east of Japan?
- The Pacific Ocean
- The Atlantic Ocean
- The Arctic Ocean
- The Indian Ocean
-
Which tectonic plate was pushed beneath Japan during the 2011 Tōhoku earthquake?
- The Eurasian Plate
- The Nazca Plate
- The Indian Plate
- The Pacific Plate
-
What was the magnitude of the Tōhoku earthquake on 11 March 2011?
- 6.3
- 8.0
- 7.8
- 9.0
-
What was the approximate death toll of the 2011 Tōhoku earthquake and tsunami?
- About 8,900
- About 18,500
- About 1,850
- About 185,000
-
Which nuclear power station was affected by the 2011 tsunami in Japan?
- Fukushima
- Chernobyl
- Sellafield
- Three Mile Island
-
Tōhoku was magnitude 9.0 and Nepal was 7.8. Why did Tōhoku release far more energy?
- The magnitude scale is logarithmic, so 1.2 steps higher means many times more energy
- Magnitude 9.0 is simply 1.2 times larger than 7.8, so it releases only slightly more energy
- Nepal's quake was measured on a different scale altogether
- Tōhoku lasted for a much shorter time than Nepal's quake
-
A tsunami wave reached 40 metres in places. Which type of factor is this?
- Human
- Physical
- Social
- Economic
-
A nuclear power station on a coast was damaged in the disaster. Which type of factor is this?
- Geological
- Physical
- Human
- Climatic
-
Which sequence correctly shows how the Tōhoku tsunami formed?
- The sea floor jolts up, a wave races to the shore, the plate slips, and water spreads out over the land
- Water spreads out, the plate slips, the wave races, the sea floor jolts up
- The plate slips under Japan, the sea floor jolts up, water spreads out, and a wave races to the coast
- A wave races to the coast, water spreads out, the sea floor jolts up, the plate slips
-
Why did a wealthy, well-prepared country like Japan still suffer so many deaths in 2011?
- Japan had no earthquake drills at all, unlike Nepal
- Nepal's earthquake was far stronger than Japan's
- Its tsunami reached a densely populated coast, overwhelming some defences despite Japan's wealth
- Japan's homes were all built from mud and straw, which is why the tsunami destroyed every one of them
-
A sea wall was built to protect a Japanese town. Which statement best evaluates it?
- It saved lives from smaller waves but was overtopped by the largest tsunami
- It had no effect, because walls cannot resist water at all
- It made the tsunami stronger by blocking the water, so the waves rose higher against the town
- It stopped all water from entering the town in every case
-
Which statement correctly compares the 2011 Japan and 2015 Nepal earthquakes?
- Both were major quakes at destructive boundaries, but Japan's deaths came mostly from the tsunami
- Both were tsunamis caused by volcanoes on land, which erupted under the sea near the coast and flooded the cities
- Japan's quake happened in the middle of a plate, far from any boundary
- Nepal's quake happened at a constructive boundary
-
Why can a wealthy country still suffer many deaths from an earthquake?
- Earthquakes only cause deaths in countries that sit directly on fault lines
- Wealth and preparation do not remove vulnerability, as hazard scale matters
- Earthquake deaths depend only on what time of day the shock happens
- Richer countries always construct weaker buildings than poorer countries do
-
Why is vulnerability a better way to explain disasters than magnitude alone?
- It replaces the need to study the physical hazard at all
- It considers how exposed and prepared people are, not just the size of the hazard
- It measures the magnitude of a hazard in the same way as a seismometer
- It shows only how much money a country spends on aid, and nothing about how safe its buildings are
-
Which evaluation of preparation in Japan is most accurate?
- Preparation only affects shaking, and never affects the sea
- Preparation was useless because it saved no lives at all
- Drills and sea walls saved many lives, but preparation cannot fully protect against the largest events
- Preparation fully removed all risk from the tsunami, so no one needed to leave the coast or move to higher ground at all
-
Why might Nepal's 2015 earthquake show different human factors from Japan's 2011 tsunami?
- Japan had no coastline, so the tsunami caused no damage to any town, port or nuclear power station anywhere at all in 2011
- Nepal had no buildings, so the earthquake caused no damage
- Both had identical human factors and identical physical hazards
- Nepal's risk came from weak buildings and poverty, while Japan's came from a high-exposure coast and huge waves
-
Which statement best explains the impact of the Tōhoku disaster?
- A small surface quake had no tsunami, so the damage was limited
- A huge undersea quake created a tsunami that hit a densely built coast, with nuclear risk, despite good preparation
- A drought caused the wave, which hit a sparsely populated coast
- A volcano erupted under the sea and dried the coast, so the sea water never reached the towns or the ports at any point during the whole disaster
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