Chapter 2 Flashcards
Seafloor spreading is ____.
the lateral movement of the oceanic lithosphere near spreading centers
A lithospheric plate is composed of ____.
the upper rigid mantle (80 to 100 km) capped by either oceanic or continental crust
____ plate boundaries are where tectonic plates move toward one another; ____ plate boundaries are where the plates slide past each other; divergent plate boundaries are where plates move away from each other.
convergent
transform
The characteristics listed below apply either to active or passive margins. Select all the characteristics of active margins.
- ocean trenches possible
- modified by tectonic movement and volcanoes
- broad and shallow with thick sedimentary deposits
- known as a trailing margin
- represents a plate boundary
- ocean trenches possible
- modified by tectonic movement and volcanoes
- represents a plate boundary
____ result in volcanic activity that may operate independently of plate boundaries. These volcanoes can form anywhere on a tectonic plate.
Hotspots
The lateral movement of the oceanic lithosphere near ocean ridges is called seafloor ____.
spreading
The Hawaiian Islands to the west of the main island have inactive volcanoes because they have moved off of the ____.
hotspot
Each lithospheric ____ consists of the upper 80 to 100 km of rigid mantle rock and is topped by either oceanic or continental crust.
plate
Guyots (flat-topped seamounts) are the result of ____.
volcanic islands being eroded after moving off the hotspot that formed them
Plates are moving apart.
divergent
Plates are moving toward one another.
convergent
Plates are sliding past each other.
transform
If you know the age of the rocks on a particular seamount and the distance it is from its associated hotspot, you can determine the rate of ____ motion.
plate
The relatively calm trailing edge of continents are called ____ margins, while the leading edge of continents are called ____ margins.
passive; active
Reason: Active margins may also be called Pacific-style and passive margins may be called Atlantic-style.
A hot spot located near a diverging plate boundary can produce a ____ ridge, which is a continuous series of seamounts very close together.
transverse or aseismic
Hotspot volcanoes are likely the result of ____.
rising magma from the mantle
Reason: The chemistry of hotspot magma suggests a possible start at the core-mantle boundary.
The Hawaiian Island chain is the result of a ____.
volcanic hotspot
Volcanic islands in the ocean that move off of the hotspots that formed them will ____.
be worn down by water and wave erosion to form flat-topped seamounts (guyots)
Reason: Erosion will reduce the top of the island until it is below the wave base of erosion.
True or false: Since hotspots operate independently of the plate tectonic system, they are not useful for studying plate motion.
False
Reason: The rates and direction of plate motion can be determined by how fast and in what direction the plate moves away from a hotspot since the rocks farther away from the hotspot are older than the closer rocks.
A continuous series of seamounts very close together formed from a hotspot near a spreading center is called a ____ ridge.
transverse
Reason: Transverse ridges are also called aseismic ridges.