Environmental Management - 0680 CIE

Earthquakes And Volcanoes

Akopọ

The ground beneath your feet feels solid and still, yet the Earth's outer shell is broken into vast slabs that creep, grind and pull apart all the time. Where these tectonic plates meet, the planet releases its energy in two of the most dramatic natural hazards we know: earthquakes that can level a city in seconds, and volcanoes that build mountains and darken skies. The same forces that put millions of people at risk also create some of the most fertile farmland and spectacular scenery on Earth.

In this lesson you will learn why earthquakes and volcanoes cluster where they do, how the three types of plate boundary work, and what actually happens during an eruption. You will then follow the exam-ready chain that Environmental Management questions always reward: the causes of a tectonic event, its impacts on people and the environment, and the strategies used to manage it before, during and after, illustrated by real disasters such as the 2010 Haiti earthquake and the 2011 Japan earthquake and tsunami.

Awọn Afojusun

  1. 6.1.1 Describe the structure of the Earth, limited to: (a) crust (b) mantle (c) core.
  2. 6.1.2 Identify the Earth’s continents: Africa, Antarctica, Asia, Europe, North America, Oceania and South America.
  3. 6.1.3 Describe and explain the distribution of earthquakes and volcanoes, limited to: (a) tectonic plates and their movement (b) hotspots.
  4. 6.1.4 Describe how convection currents in the mantle result in plate movements that cause earthquakes and the formation of volcanoes, limited to: (a) divergent or constructive plate boundaries: plates move apart causing volcanic activity and earthquakes (b) convergent or destructive plate boundaries: subduction of one plate beneath another causing earthquakes and a line of volcanoes (c) conservative plate boundaries: plates slide past each other causing earthquakes.
  5. 6.1.5 Describe the features of earthquakes, limited to: (a) release of energy (b) focus (c) epicentre (d) magnitude: Moment Magnitude Scale.
  6. 6.1.6 Describe the features of volcanic eruptions, limited to: (a) magma rising to the surface to form lava (b) ash (c) gases: water vapour, carbon dioxide and sulfur dioxide (d) acid rain (e) volcanic bombs (f) pyroclastic flows.
  7. 6.1.7 Describe and explain the impacts of tectonic events on people and the environment, limited to: (a) damage to buildings and infrastructure (b) loss of crops, livestock and habitats (c) evacuation of people and livestock (d) fire (e) tsunamis (f) landslides (g) contamination of drinking-water supplies (h) water-related disease (i) financial losses (j) human health.
  8. 6.1.8 Describe strategies for managing the impacts before, during and after a tectonic event, limited to: (a) monitoring and warning (b) land use zoning (c) structure of buildings (d) disaster preparation (plans, drills, emergency supplies and emergency rescue teams) (e) evacuation (f) shelters (g) rebuilding of damaged areas (h) international aid.
  9. 6.1.9 Discuss the benefits and limitations of strategies for managing the impacts before, during and after a tectonic event.
  10. 6.1.10 Describe and explain the opportunities provided by volcanoes to people, limited to: (a) fertile soils (b) extraction of minerals (c) building materials (d) geothermal power (e) tourism.

Akọ̀wé Ẹ̀kọ́

Around a quarter of the world's people live close enough to a plate boundary to feel its power. A single earthquake can kill more than a hundred thousand people in under a minute, while a major eruption can ground aircraft across a continent and cut harvests for years. Yet many of these communities choose to stay, drawn by rich volcanic soils, geothermal energy and tourism. Understanding the science lets us predict, prepare for and reduce the harm, which is exactly what the exam asks you to do: link cause to impact to management.

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Oriire fun ipari ẹkọ lori Earthquakes And Volcanoes. Ni bayi ti o ti ṣawari naa awọn imọran bọtini ati awọn imọran, o to akoko lati fi imọ rẹ si idanwo. Ẹka yii nfunni ni ọpọlọpọ awọn adaṣe awọn ibeere ti a ṣe lati fun oye rẹ lokun ati ṣe iranlọwọ fun ọ lati ṣe iwọn oye ohun elo naa.

Iwọ yoo pade adalu awọn iru ibeere, pẹlu awọn ibeere olumulo pupọ, awọn ibeere idahun kukuru, ati awọn ibeere iwe kikọ. Gbogbo ibeere kọọkan ni a ṣe pẹlu iṣaro lati ṣe ayẹwo awọn ẹya oriṣiriṣi ti imọ rẹ ati awọn ogbon ironu pataki.

Lo ise abala yii gege bi anfaani lati mu oye re lori koko-ọrọ naa lagbara ati lati ṣe idanimọ eyikeyi agbegbe ti o le nilo afikun ikẹkọ. Maṣe jẹ ki awọn italaya eyikeyi ti o ba pade da ọ lójú; dipo, wo wọn gẹgẹ bi awọn anfaani fun idagbasoke ati ilọsiwaju.

  1. Which layer of the Earth contains the convection currents that move the tectonic plates? A. Crust B. Mantle C. Outer core D. Inner core Answer: B
  2. At which type of plate boundary do plates slide past each other, causing earthquakes but no volcanoes? A. Constructive B. Destructive C. Conservative D. Collision Answer: C
  3. The point on the Earth's surface directly above the origin of an earthquake is called the: A. Focus B. Fault C. Epicentre D. Magnitude Answer: C
  4. Which volcanic hazard is a fast-moving, super-hot cloud of gas and ash? A. Lava flow B. Pyroclastic flow C. Acid rain D. Ash fall Answer: B
  5. Which of the following is an opportunity provided by volcanoes? A. Pyroclastic flows B. Geothermal power C. Tsunamis D. Acid rain Answer: B

O wa lori ohun elo Green Bridge

Gba ohun elo Green Bridge CBT sori foonu tabi kọmputa rẹ lati ri awọn akọsilẹ ẹkọ ni kikun, awọn ibeere adaṣe, ati diẹ sii.

Awọn akọsilẹ ẹkọ ni kikun pẹlu awọn aworan apejuwe
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Kọ ẹkọ laisi intanẹẹti, nigbakugba, nibikibi
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O wa lori ohun elo Green Bridge

Gba ohun elo Green Bridge CBT sori foonu tabi kọmputa rẹ lati ri awọn akọsilẹ ẹkọ ni kikun, awọn ibeere adaṣe, ati diẹ sii.

Awọn akọsilẹ ẹkọ ni kikun pẹlu awọn aworan apejuwe
Oluranlọwọ ẹkọ ti AI ṣe agbara rẹ
Kọ ẹkọ laisi intanẹẹti, nigbakugba, nibikibi
O wa lori Android, Windows, macOS, ati Linux

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