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“Building” Features on Earth's Surface

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“Building” Features on Earth’s Surface



Plate tectonics



Tectonics comes from the

Greek word tekton which

means builder.



Plate tectonics refers to

the building of features

on Earth’s surface due to

deformation caused by

plate movements.

“Building” Features on Earth’s Surface



Plate movements create

mountain ranges, trenches

and rift valleys at or near

plate boundaries.



There is a relationship

between volcanoes and

plate boundaries, and

earthquakes and plate

boundaries.

“Building” Features on Earth’s Surface

•Oceanic trenches are created when one plate goes under

another (subduction.)

•The valley above the subduction zone is called a “trench”

“Building” Features on Earth’s Surface



Trenches can be over 10,000

meters deep.

•They are common in the western

Pacific where there is ocean-

ocean subduction.



•A long trench is located along the

west coast of South America,

where the Nazca Plate is being

subducted under the continent.

“Building” Features on Earth’s Surface

Volcanoes at Plate Boundaries

Volcanoes are

common along mid-

ocean ridges and

subduction zones,

where they form

volcanic arcs (volcanic

islands)

“Building” Features on Earth’s Surface

Volcanoes at Plate Boundaries

Magma is produced above

the subducted plate and

rises toward the surface.



Magma rises because it is

less dense than the

surrounding rock.

“Building” Features on Earth’s Surface



Volcanoes at Plate Boundaries



The “Ring of Fire” around the Pacific Ocean is caused by this

melting at subduction zones.

“Building” Features on Earth’s Surface



Volcanoes at Plate Boundaries

“Building” Features on Earth’s Surface



Hot Spots



“Hot spots” begin at the

boundary between the mantle

and outer core.



These are narrow columns of

hot mantle material.

They rise to the surface,

creating hot spot volcanoes.

“Building” Features on Earth’s Surface



Hot Spots

“Building” Features on Earth’s Surface



Hot Spots

Some hot spots are located under continents.



-The Rift Valley in Africa

“Building” Features on Earth’s Surface



Hot Spots

Some hot spots are located under continents.



-Yellowstone National Park

“Building” Features on Earth’s Surface



Hot Spots

“Building” Features on Earth’s Surface



Mountains at Plate Boundaries

Large mountain ranges are often located near convergent plate

boundaries.

“Building” Features on Earth’s Surface



Mountains at Plate Boundaries



Himalayas between India and China



Alps in Europe



Andes in South America



Coastal mountain ranges in the western United States

“Building” Features on Earth’s Surface



Mountains at Plate Boundaries

Mountains are built in two ways.

1. Magma forms chains of

volcanoes which are mountains.



2. When two plates are pushed

together and stacked on top of

each other.

“Building” Features on Earth’s Surface

Growth of Continents at Subduction Zones

“Building” Features on Earth’s Surface



Growth of Continents at Subduction Zones



Continental accretion:

When two plates meet and one is subducted

(goes under the other,) layers of sediment are

scraped off the plate that goes under.



The material (layers of sediment) is turned into

rock by heat and pressure.



The material makes the continent grow larger.

“Building” Features on Earth’s Surface

Growth of Continents

Continents also grow because of volcanoes and batholiths.

“Building” Features on Earth’s Surface



Earthquakes and Plate Tectonics



Plates moving past each other do not

always slide smoothly.



Transform faults that are on land or

close to land can be dangerous to

people.



Ex. San Andreas Fault

“Building” Features on Earth’s Surface



Earthquakes and Plate Tectonics

“Building” Features on Earth’s Surface



Earthquakes and Plate Tectonics

“Building” Features on Earth’s Surface



Earthquakes and Plate Tectonics

Earthquakes at subduction

zones and continent-

continent collision zones

are also dangerous for

people.



The Pacific Rim is an

example.

Another area stretches

from the Mediterranean to

southeast Asia.

“Building” Features on Earth’s Surface

Earthquakes and Plate Tectonics

Earthquakes in subduction zones can be shallow, near the

trench, up to as deep as hundreds of kilometers.



Earthquakes near continent-continent collision zones can effect

large areas as one continent is pushed under the other.

“Building” Features on Earth’s Surface

Earthquakes and Plate Tectonics

“Building” Features on Earth’s Surface

Earthquakes, Tsunamis, and Plate Tectonics



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