Tectonics Flashcards
(125 cards)
Where is the Continental Crust located
- Beneath Earth’s continents
- -Extends under shallow seas near continents
- -Thicker but less dense than oceanic crust
What is the Continental Crust made of?
- Consists mainly of lighter rocks like granite
- Forms large landmasses
- Less dense than basalt
How old is the Continental Crust?
- Wide range of ages
- From very recent to nearly 4 billion years old
- Older on average than oceanic crust
Why do tectonic plates move?
*Due to convection currents in the mantle
* Heat from Earth’s core drives mantle flow
* Mantle material (asthenosphere) in motion drives plate movement
What happens to the mantle material when it gets heated by Earth’s core?
- Becomes less dense and expands
- Rises and spreads beneath tectonic plates
- Causes plates to move apart (diverge)
What happens to mantle material as it cools?
- Becomes denser and contracts
- Sinks back towards the core
- Pulls tectonic plates along with it
What is the slab pull force, and how does it affect tectonic plates
- Occurs when a denser oceanic plate subducts
- Gravity pulls the plate into the mantle
- Pulls the rest of the plate, driving further convergence
What is sea floor spreading, and how does it create new oceanic crust?
- Happens when two oceanic plates diverge
- Magma rises to fill the gap between plates
- New oceanic crust forms as magma cools and solidifies
How does magnetic striping provide evidence for sea floor spreading?
- Basaltic rocks align with Earth’s magnetic field as they cool
- Alternating patterns of normal and reversed polarity
- Shows history of Earth’s magnetic field
- Confirms continuous formation of new crust at mid-ocean ridges
What happens during normal and reverse polarity, and how does it relate to Earth’s magnetic field?
- Normal polarity: Magnetic North points towards geographic North
- Reverse polarity: Magnetic North points towards geographic South
- Earth’s magnetic field has reversed many times
- Recorded in alignment of magnetic minerals in oceanic crust
What is magnetic striping, and how does it relate to plate tectonics?
- Pattern of alternating magnetic alignments in basaltic rocks
- Iron-rich minerals align with Earth’s magnetic field as they cool
- Symmetrical stripes on either side of mid-ocean ridges
- Evidence for sea floor spreading and tectonic plate movement
What happens when two oceanic plates move apart?
- Two oceanic plates move apart (diverge).
- Decreased pressure causes parts of the underlying mantle to melt, forming magma.
- Magma rises through the gap to the Earth’s surface and fills the space created by the spreading plates.
What are the results of Oceanic-Oceanic Divergence?
- Basaltic rocks form new oceanic crust as magma cools and solidifies.
- A deep rift valley with steep sides forms at the center of the ridge.
- Magma can create underwater volcanoes.
- Over time, volcanoes may break the ocean surface to form volcanic islands (e.g., Surtsey, Iceland).
What happens when two continental plates move apart?
- Two continental plates move apart (diverge).
- Rocks stretch and fracture, creating parallel faults.
- The land between these faults collapses to form a deep rift valley with steep sides.
- Decreased pressure in the mantle causes it to melt, forming magma.
Magma can rise through weak areas in the crust, forming volcanoes.
What is an example of Continental-Continental Divergence?
- The Nubian Plate pulls apart from the Somalian Plate, forming the Great Rift Valley (e.g., Mount Kenya, Mount Kilimanjaro).
What happens when two continental plates collide?
- Two continental plates collide.
- Neither plate subducts because both are light and buoyant.
- Enormous compressional pressure causes rock layers to buckle and fold, forming fold mountains.
- Friction along the convergent boundary causes earthquakes.
- No magma rises to the surface, so no volcanoes are formed.
What are examples of Continental-Continental Convergence?
- Young fold mountains: The Himalayas (Indian Plate and Eurasian Plate).
- Old fold mountains: Appalachian Mountains (USA).
What happens when an oceanic plate converges with a continental plate?
- The denser oceanic plate subducts under the less dense continental plate.
- The point of collision is the subduction zone, forming an oceanic trench.
- High pressure in the subducted plate causes water to be released, lowering the melting point of the mantle above and forming magma.
- Magma rises through faults in the crust to form volcanoes.
- Enormous compressional pressure causes rock layers to buckle and fold, forming fold mountains.
- Earthquakes can occur due to friction along the subducting oceanic plate.
What is an example of Oceanic-Continental Convergence?
- Oceanic Nazca Plate converges with continental South American Plate, forming the Peru-Chile Trench, Andes Mountains, Nevado del Ruiz volcano, and the 2010 Chile earthquake.
What happens when two oceanic plates converge?
- The older, denser oceanic plate subducts under the less dense oceanic plate.
- The point of collision forms a subduction zone, creating an oceanic trench.
- High pressure in the subducted plate causes water to be released, lowering the melting point of the mantle above and forming magma.
- Magma rises through faults in the overriding plate to form volcanoes.
- A chain or arc of volcanic islands forms.
- Earthquakes can occur due to friction along the subducting oceanic plate.
What is an example of Oceanic-Oceanic Convergence?
- Pacific Plate converges with Eurasian Plate, forming the Mariana Trench and volcanic islands like Guam.
What happens at a Transform Plate Boundary?
- Plates slide past one another horizontally.
- No formation of volcanoes.
- Earthquakes can occur due to the friction between the sliding plates.
What is an example of a Transform Plate Boundary?
- Pacific Plate slides past the North American Plate, forming the San Andreas Fault in California, USA, where earthquakes like the 1989 Loma Prieta earthquake are common.
What happens at divergent plate boundaries to form shield volcanoes?
- Plates move apart, causing the crust to stretch and develop fractures.
- Decreased pressure causes parts of the underlying mantle to melt, forming magma.
- Magma contains dissolved gases and is less dense than the surrounding materials.
- Magma rises through the cracks in the crust to the Earth’s surface, erupting as lava.
- Over successive eruptions, a volcano forms with layers of lava.
- The lava travels longer distances before cooling and solidifying, creating a volcano with gentle sloping sides and a broad summit.
- In some cases, the summit may be blown off during a violent eruption, resulting in an enlarged crater known as a caldera.