Plate Tectonic Theory
Evidence for Plate Tectonic Theory
Hydrothermal Vent
Isotasy
Features and how theyre formed
100

What is Earth's Crust/Lithosphere made of ?

Plates

100

What was described that the plates fit like?

a puzzle 

100

very hot, acidic (low pH), emits hydrogen sulfide, high pressure, no light, and very rich in minerals such as copper, zinc, iron, maganese, etc.

physical characteristics/features/ properties of a hydrothermal vent.

100

buoyant properties of layering rocks, which float on other layers, according to their density and thickness. 

what is isostasy 

100

State what happens during a convergent/divergent plate boundary, where it happens, stress type and features. 

(plates move apart of each other) Constructive plate boundaries occur when two plates move away from each other. 

North American and Eurasian Plate 

Tension

Features: earthquakes , ocean ridges, volcanoes

200

What does plate movement cause?

earthquakes, mountain building and volcanic erruptions. 

200

What is paleontology?

Related fossils on continents separated by ocean shows they were once joined. 

200

Where do hydrothermal vents form?

typically on mid ocean ridges, where Earths tectonic plates are spreading apart and where magma wells up to the surface or close beneath the seafloor. 

200

What does isostasy explain?

why the earth's crust floats on the denser, underlying layer. 

200

Destructive (subduction zone)

Destructive plate boundaries occur when an oceanic plate is forced under (or subducts) a continental plate

Pacific plate and the Eurasian plate

compression 

earthquake, oceanic trenches, volcanoes, destructive with 2 oceanic plates, island arcs 

300

What do plates move due to?

convection currents in the asthenosphere

300

how were mountain ranges evidence for the plate tectonic theory?

stratification/layering of mountain range match of mountains found on different continents indicating continents were once joined together.

300

how many steps are in the formation of hydrothermal vents?

5

300

What does the principle of isostasy show?

The principle of isostasy shows that the Earth’s crust is generally higher where it is thicker and less dense; lower where it is thinner and denser.

300

Conservation (transform) 

conservative plate boundaries occur when 2 plates slide past each other 

North American plate and the pacific plate

shearing 

earthquake, faulting 


400

What do continents lie on?

Plates

400

Mapping of the seafloor

what is sonar

400

how do hydrothermal vents form? 

1. crack in the seafloor where water seeps in

2. water is superheated by the underlying hot magma

3. hot water builds up pressure, causing it to rise out of cracks 

4. dissolves minerals on the way out 

5. some minerals precipitate out along edge of crack forming a vent. 

400

Which crust is less dense between continental and oceanic. 

Continental crust is less dense as compared to oceanic crust (at convergent boundaries, oceanic will subside – go under cont.).

400

collision

collision plate boundaries occur when 2 continental plates move towards each other

indo-australian and the Eurasian plate

compression 

earthquake, fold mountains 

500

What boundaries do plates meet at?

convergent, divergent and transform

500

what is seen at mid ocean ridges that provides us with evidence for the plate tectonic theory?

magnetic reversal of rocks

500

why are hydrothermal vents important ?

support unique ecosystems and their communities of organisms in the deep ocean. 

500

how do boundaries form

plates move apart, magma rises and cools to make new crust