Hazardous Eath Plate boundarirs Flashcards
Divergent (Constructive) Plate Boundary
Plates Move apart At MID-OCEAN RIDGES
MAGMA rises through ASTHENOSPHERE onto the SEA FLOOR the ERUPTION OCCURS the MAGMA is cooled RAPIDLY -Forms PILLOW LAVAS
MAGMA continues to RISE to LITHOSPHERE putting it under EXTREME PRESSURE which PRODUCES UNDERWATER RIFT VALLEYS
Mid-Ocean Ridge
Depth of 2.5km
Long CHAINS of MOUNTAINS rising ABOVE the SEA BED
They are NOT CONTINUOUS and BROKEN in SEGMENTS by TRANSFORM FAULTS -there is no VOLCANIC ACTIVITY here
However ENERGY can Be RELEASED can cause EARTHQUAKES
SEA WATER can SEEP into MID-OCEAN RIDGES and be SUPERHEATED CHANGING the CHEMISTRY
Named example Divergent Plate Boundary
Mid Atlantic-Ridge
EURASIAN moves away from NORTH AMERICA PLATE
Convergent Plate Boundaries types
Oceanic -Oceanic
Oceanic -continental
Continental Continental
Convergent Plate Boundary -Oceanic-Continental
When Two Plate collide TOGETHER
The Denser of the Plate will SUBDUCT, which creates an OCEAN TRENCH
The SEDIMENTS and ROCK CRUMPLE on the Oceanic Plate which UPLIFTS the CONTINENTAL PLATE where
MOLTEN MATERIAL is INJECTED into it - creates MOUNTAIN CHAINS
FAULTING and FRACTURING occurred in the BENIOFF ZONE -which RELEASES ENERGY creating EARTHQUAKES
Convergent Plate Boundary Oceanic-Continental - Example
Andes in Pacific Coast of South America
Convergent Plate Boundary- Oceanic Oceanic
The Denser of the Two Oceanic Plates Subducts
The SUB-DUCTED PLATE MELTS causing MAGMA to Rise, which FORMS VOLCANIC ISLANDS - ISLAND ARCS
Convergent Plate Boundary- Oceanic Oceanic Example
NORTH AMERICA PKATE SUB-DUCTS under CARIBBEAN PLATE - creates ANTILLES
Convergent Plate Boundary- Continental Continental
Two Continental Plates CONVERGE very LITTLE if ANY SUBDUCTION
DUE to them having SIMILAR DENSITIES
Convergent Plate Boundary- Continental Continental Example
African and Eurasian plates CREATED the ALPS