Earth’s Layers
Plate Boundaries & Movements
Plate Tectonics Evidence
Hot Spots & Mantle Processes
Active vs. Passive Margins
100

Compisitional Layers

V.S

Functional Layers

Crust, Mantle and Core

V.S

Lithsophere and Asthenosphere

100

Divergent boundary

Plates move away from each other

100

What are Plate Techtonics

Edge of tectonic plate where plate interactions occur

100

Seafloor spreading

Magma pushing up to push the plates away from each other (Ocean divergent)

100

Active margin

Where plates are actively moving

200

Lithsophere v.s. Asthenosphere

Crust and upper mantle vs lower mantle

200

Convergent boundary

2 plates come together and collide

200

Continental rift

Continental divergent plate boundary

200

Hot spot

Rising plumes of mantle material in the middle of a plate

200

Passive margin


Plates are not moving/no activity

300

What are the functional (mechanical) layers of the earth? How are they different from the

compositional layers?

Lithosphere and asthenosphere; different from compositional because they are organized by how they behave

300

Transform boundary

2 plates slide past each other

300

Where is new crust created? Destroyed? And why for each?

Created due to magma upwelling on divergent plates, and destroyed at oceanic convergent due to subduction

300

Plate-mantle convection

Convection currents in the asthenosphere move lithosphere at the surface

300

What is the difference between active and passive margins? What are some examples of each?

  • Active margins move (western coast of N and S America) while passive don’t (eastern coast of N and S America)

400

Subduction

Oceanic lithosphere sinks into the asthenosphere

400

Be able to determine the type of plate boundary from a map/image

To determine the type of plate boundary from a map or image, look for patterns of earthquakes, volcanoes, mountain ranges, and ocean trenches, which are characteristic of convergent, divergent, and transform boundaries.

400

What are the two major models for the mechanism of plate tectonics?

Seafloor spreading and hotspots

400

Why do mid-ocean ridges form?

Seafloor spreading; oceanic divergent plates

400

Seafloor spreading

Magma pushing up to push the plates away from each other (Ocean divergent)

500

Why does subduction occur?

Oceanic plates are extremely dense so they sink under other plates

500

Describe the characteristics of each type of boundary, including the 3 types of convergent

boundaries and both divergent. What features are associated with each? What is the

mechanism or cause for the major features?

  • Divergent Boundaries: Plates move away from each other, forming ridges, rift valleys, and new crust via seafloor spreading.

  • Convergent Boundaries: Plates move toward each other, leading to subduction (oceanic-continental and oceanic-oceanic), mountain formation (continental-continental), and features like trenches, volcanic arcs, and island chains.

  • Transform Boundaries: Plates slide past each other, creating faults and earthquake activity.


500

What is the surface evidence for plate tectonics (in addition to those of continental drift)?

  • Earthquakes, volcanos, mountain ranges, oceanic ridges, ocean trenches

500

Slab-pull & slab-push model

Descending oceanic crust pulls the plate while elevated ridge system pushes the plate

500

Explain the continental drift hypothesis. What evidence was there? Why was it abandoned?

ontinents “drifted” to current positions. Abandoned due to lack of mechanism to explain