Humanities Alive 8 VC 3E

FIGURE3 The 10 largest earthquakes and 10 most destructive tsunamis in recorded history

Tohoku, Japan 11 March 2011 9.0 magnitude

Kamchatka, Russia 4 November 1952 9.0 magnitude

ARCTIC OCEAN

Prince William Sound, Alaska 28 March 1964 9.2 magnitude

Lisbon, Portugal 1 November 1755

Ryuku Islands, Japan 24 April 1771

Rat Islands, Alaska 2 April 1965 8.7 magnitude

Assam and Tibet 15 August 1950 8.6 magnitude

Sanriku, Japan – 15 June 1896

Tohoku, Japan – 11 March 2011

ATLANTIC

Ise Bay, Japan – 18 January 1586

Tropic of Cancer

Sumatra, Indonesia 28 March 2005 9.1 magnitude

Enshunada Sea, Japan – 20 September 1498

OCEAN

Nankaido, Japan – 28 October 1707

PACIFIC

Equator

Sumatra, Indonesia 26 December 2004

Off the coast of Ecuador 31 January 1906 8.8 magnitude

Krakatau, Indonesia 27 August 1883

Tropic of Capricorn

Northern Chile 13 August 1868

Sumatra, Indonesia 28 March 2005 8.6 magnitude

Top 10 most destructive tsunamis

OCEAN

Tsunami

Bio-Bio, Chile 27 February 2010 8.8 magnitude

Ranking

Top 10 largest earthquakes

Valdivia, Chile 22 May 1960 9.5 magnitude

0

2000

4000 km

Earthquake

Ranking

Source: Map drawn by Spatial Vision

SkillBuilder discussion Geographical inquiry 1. Identify and list the five largest earthquakes. 2. Identify and list the five most destructive tsunamis. 3. Choose one earthquake and one tsunami from your responses to questions 1 and 2 and research these events. Provide an outline of the economic, social and environmental impact of your chosen disasters.

Liquefaction Liquefaction occurs when soil suddenly loses strength and, mixed with groundwater, behaves like a liquid. This usually occurs as a result of ground shaking during a large earthquake. The types of soils that can liquefy include loose sands and silts that are below the water table, so all the space between the grains is filled with water. Dry soils above the water table will not liquefy. Once a soil liquefies, it cannot support the weight of the dry soil, roads, concrete floors and buildings above it. The liquefied soil comes to the surface through cracks, which it widens.

FIGURE4 Cars swallowed by liquefied soil on a road in Christchurch, New Zealand, 2011

Source: © Photography by Mark Lincoln

392 Jacaranda Humanities Alive 8 Victorian Curriculum Third Edition

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