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Structure of the earth. Type of Crust. LEDC. Thinner , less dense /lighter. Oceanic. MEDC. Restless Earth Topic 1. Case Studies. Predict, prepare, relief. Continental. Volcanoes. - PowerPoint PPT Presentation
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Restless Earth
Topic 1
Structu
re of the earth
Type of CrustOceanic
Continental
Thicker, less dense /lighter
Thinner, less dense /lighter
Plate boundaries
Plates pushing together
Destructive plate boundaries:
Conservative plate
boundaries:
Plates rubbing past each other
Constructi
ve plate
boundaries:
Plates pulling apart
Conv
ectio
n cu
rrent
s: cu
rrent
in
the m
ante
l tha
t mov
e plat
es
Volcanoes
Types
Shield
They are low, with gently sloping sides.They are formed by eruptions of thin, runny lava.Eruptions tend to be frequent but relatively gentle
Composite
made up of alternating layers of lava and ash. Eruptions are explosive/ pyroclastic, hot steam, ash, rock and dust
Case Studies
LEDCMEDC
Pred
ict, p
repa
re, r
elie
f
Destructive plate boundary
Destructive plate boundary
Oceanic plate and Continental plates push together, creating volcanoes
Continental and Continental plates push together – creating fold mountains
Example: Nazca and South American plates
Constructive plate boundary
Plates pull apart creating volcanoes and earthquakes
EXAMPLE: Eurasian and North American Plates
Conservative Plate Boundary
Plates push past each other. They can be traveling in different directions
Or in the same direction but one is faster than the other.
Cause Earthquakes
Example north American plate and the pacific plate
Plate boundaries
Constructive Plate Boundary
Destructive Plate Boundary
Conservative Plate Boundary
The structure of the earth
What are the layers of the earthHow hot are they
Are they solid or liquid
4 layers• The inner core is in the centre and is the
hottest part of the Earth. It is solid and made up of iron and nickel with temperatures of up to 5,500°C. With its immense heat energy, the inner core is like the engine room of the Earth.
• The outer core is the layer surrounding the inner core. It is a liquid layer, also made up of iron and nickel. It is still extremely hot, with temperatures similar to the inner core.
• The mantle is the widest section of the Earth. It has a diameter of approximately 2,900 km. The mantle is made up of semi-molten rock called magma. In the upper parts of the mantle the rock is hard, but lower down the rock is soft and beginning to melt.
• The crust is the outer layer of the earth. It is a thin layer between 0-60 km thick. The crust is the solid rock layer upon which we live.
Shield Volcanoe
They are low, with gently sloping sides.They are formed by eruptions of thin, runny lava.Eruptions tend to be frequent but relatively gentleExample: Hawaii
Composite volcano
Composite Volcanoes are made up of alternating layers of lava and ash. Eruptions are explosive/ pyroclastic, hot steam, ash, rock and dust
Example: Mount Pinatubo Philippines
Earthquake
Movement of ground cases by release of energy from a sudden shift of rocks in the earths crust
Epicentre
The point below Earths surface where movement of rock produces
an earthquake
Focus
• The point below earth’s surface where movement of rock produces a
earthquake
Aftershock
A smaller earthquake that occurs after a larger
earthquake
Magnitude
The measurement of the total strength or amount of energy
release by an earthquake
Richter scale
A measurement of the magnitude of an earthquake based on the readings of a seismography. It ranges from 0-9.
(each number represents a 10 fold increase in ground motion)