10-2
... 25. Name three areas where plate boundaries may be located. _______________________________________________________________ _______________________________________________________________ _______________________________________________________________ ________________________________________________ ...
... 25. Name three areas where plate boundaries may be located. _______________________________________________________________ _______________________________________________________________ _______________________________________________________________ ________________________________________________ ...
plate tectonics - Science with Ms. Reathaford!
... broken into large slabs of rock, called plates, which moves in different directions at different speeds. These plates interact with one another at plate boundaries. Each type of boundary has specific characteristics and processes associated with it. ...
... broken into large slabs of rock, called plates, which moves in different directions at different speeds. These plates interact with one another at plate boundaries. Each type of boundary has specific characteristics and processes associated with it. ...
Plate Tectonics: Earth`s Plates and Continental
... Ocean Crust meets Continental Crust –Because continental crust is lighter than oceanic crust, continental plates ”float” higher. –So when an oceanic plate meets a continental plate, it slides under the lighter plate and down into the mantle. The slab of oceanic rock melts when the edges get to a de ...
... Ocean Crust meets Continental Crust –Because continental crust is lighter than oceanic crust, continental plates ”float” higher. –So when an oceanic plate meets a continental plate, it slides under the lighter plate and down into the mantle. The slab of oceanic rock melts when the edges get to a de ...
An Introduction to the Seafloor and Plate Tectonics
... 4) Compare and contrast the differences among the major ocean basins with respect to the types of plates found in each. Introduction: The Layers of the Earth Approximately 70% of the Earth’s surface (covering 361 million square kilometers) is covered by the ocean. The average ocean depth (3800m) is ...
... 4) Compare and contrast the differences among the major ocean basins with respect to the types of plates found in each. Introduction: The Layers of the Earth Approximately 70% of the Earth’s surface (covering 361 million square kilometers) is covered by the ocean. The average ocean depth (3800m) is ...
Layers of the Earth
... Layers of the Earth • Skin of the peach is the crust • Meat of the peach is the mantle • Pit of the peach is the ...
... Layers of the Earth • Skin of the peach is the crust • Meat of the peach is the mantle • Pit of the peach is the ...
earths_interior
... particles of a substance are moving. At first, the Earth gets a little cooler as you go deeper. But at 20 meters depth, the temperature starts rising. For every 40 meters you descend, the temperature rises about 1° Celsius. After a few kilometers this rate slows a bit, but it gets hotter the d ...
... particles of a substance are moving. At first, the Earth gets a little cooler as you go deeper. But at 20 meters depth, the temperature starts rising. For every 40 meters you descend, the temperature rises about 1° Celsius. After a few kilometers this rate slows a bit, but it gets hotter the d ...
The Layer`s Of The Earth!
... the lithosphere. • The lithosphere is composed of part of the crust and the upper part of the mantle (the top 100 km). • It is composed of hard, brittle rock ...
... the lithosphere. • The lithosphere is composed of part of the crust and the upper part of the mantle (the top 100 km). • It is composed of hard, brittle rock ...
Short course program: Earth and planetary materials and dynamics
... BS: Reference frames for plate motion and true polar wander A: BS: Relation between geoid, topography, volcanism and mantle dynamics, Earth and planets Tobias Rolf (CEED, Oslo): Linking surface observations and internal dynamics through mantle convection modelling of Earth and Venus Planetary meltin ...
... BS: Reference frames for plate motion and true polar wander A: BS: Relation between geoid, topography, volcanism and mantle dynamics, Earth and planets Tobias Rolf (CEED, Oslo): Linking surface observations and internal dynamics through mantle convection modelling of Earth and Venus Planetary meltin ...
Topic 11A: Plate Tectonics, Part III Online Lecture: Types of
... Where plates run into and grind against one another, they are “squeezed” or “bent.” The pressure to move builds up, eventually overcomes friction, and the plate(s) “slip” forward and “snap” back into shape (an earthquake happens). ...
... Where plates run into and grind against one another, they are “squeezed” or “bent.” The pressure to move builds up, eventually overcomes friction, and the plate(s) “slip” forward and “snap” back into shape (an earthquake happens). ...
Inside Earth Test Study Guide
... outer core – a layer of molten iron and nickel that surrounds the inner core of the Earth inner core – a dense sphere of solid iron and nickel at the center of the Earth magnet – a material that attracts steel, iron, cobalt, and nickel Earth as a magnet – the Earth acts like a magnet because of the ...
... outer core – a layer of molten iron and nickel that surrounds the inner core of the Earth inner core – a dense sphere of solid iron and nickel at the center of the Earth magnet – a material that attracts steel, iron, cobalt, and nickel Earth as a magnet – the Earth acts like a magnet because of the ...
CH 5 section 1
... ______, twigs, litter, and small ______. Small particles of soil/rock are also found=sediment=sedimentary rock over time. 1. What would the Earth’s surface be like today if erosion were the only force acting upon it? What is erosion? 2. What are the four layers that the Earth is composed of? (Explai ...
... ______, twigs, litter, and small ______. Small particles of soil/rock are also found=sediment=sedimentary rock over time. 1. What would the Earth’s surface be like today if erosion were the only force acting upon it? What is erosion? 2. What are the four layers that the Earth is composed of? (Explai ...
The What of Plate Tectonics
... Actions at Divergent Boundaries Oceanic ridges are continuous elevated zones on the floor of all major ocean basins. The rifts at the crest of ridges represent divergent plate boundaries Rift valleys are deep faulted structures found along the axes of divergent plate boundaries. They can deve ...
... Actions at Divergent Boundaries Oceanic ridges are continuous elevated zones on the floor of all major ocean basins. The rifts at the crest of ridges represent divergent plate boundaries Rift valleys are deep faulted structures found along the axes of divergent plate boundaries. They can deve ...
adult - Old Colony Council
... a builder or architect. Plate tectonics suggests that large features on Earth’s surface, such as continents, ocean basins, and mountain ranges, result from interactions along the edges of large plates of Earth’s outer shell. This outer shell is called the lithosphere from the Greek “lithos,” meaning ...
... a builder or architect. Plate tectonics suggests that large features on Earth’s surface, such as continents, ocean basins, and mountain ranges, result from interactions along the edges of large plates of Earth’s outer shell. This outer shell is called the lithosphere from the Greek “lithos,” meaning ...
Earth_s_Interior___Convection_2010
... How do we know what is down there? • Direct Evidence – Volcanoes sending lava out from below – Rock Samples (deepest we have ever drilled is just a few miles) ...
... How do we know what is down there? • Direct Evidence – Volcanoes sending lava out from below – Rock Samples (deepest we have ever drilled is just a few miles) ...
Plate Tectonics The Earth` crust is broken into various chunks called
... chunks called “plates” These plates do not stay in one place, this movement is referred to as “Plate Tectonics” The movement is caused by the convection currents in Earth's mantle. ...
... chunks called “plates” These plates do not stay in one place, this movement is referred to as “Plate Tectonics” The movement is caused by the convection currents in Earth's mantle. ...
Plate Tectonics and Geology
... 1782 Benjamin Franklin: suggested that crust of Earth "floated" on fluid interior (crust broken and disordered by movement of fluids) ...
... 1782 Benjamin Franklin: suggested that crust of Earth "floated" on fluid interior (crust broken and disordered by movement of fluids) ...
Earth From Crust to Core
... 1. Use hard boiled eggs as a simple model of the earth’s layers. Leaving the shells on, slice eggs down the center. Give one half of an egg to each student. Ask students to find the egg equivalent to the earth’s crust, mantle and core. Discuss how the egg model is like and unlike the real earth. (Eg ...
... 1. Use hard boiled eggs as a simple model of the earth’s layers. Leaving the shells on, slice eggs down the center. Give one half of an egg to each student. Ask students to find the egg equivalent to the earth’s crust, mantle and core. Discuss how the egg model is like and unlike the real earth. (Eg ...
Seismic Reflection and Ocean Crustal Structure
... determined from ophiolite studies • Understand how oceanic crustal structure is linked to mantle melting and volcanic processes • Physics: Understand what seismic impedance is and how it controls the amplitude of seismic reflections • Data collection: airguns & LOTS of hydrophones • Data processing: ...
... determined from ophiolite studies • Understand how oceanic crustal structure is linked to mantle melting and volcanic processes • Physics: Understand what seismic impedance is and how it controls the amplitude of seismic reflections • Data collection: airguns & LOTS of hydrophones • Data processing: ...
ch 7 study guide Answers
... A mid-ocean ridge is a mountain chain found on the ocean floor. It is formed at a divergent boundary where plates are separating. The magma is pushing up through the plate boundary causing the plates to move away from each other. The youngest rock is found at the mid-ocean ridge. The rock get older ...
... A mid-ocean ridge is a mountain chain found on the ocean floor. It is formed at a divergent boundary where plates are separating. The magma is pushing up through the plate boundary causing the plates to move away from each other. The youngest rock is found at the mid-ocean ridge. The rock get older ...
Mantle plume
A mantle plume is a mechanism proposed in 1971 to explain volcanic regions of the earth that were not thought to be explicable by the then-new theory of plate tectonics. Some such volcanic regions lie far from tectonic plate boundaries, for example, Hawaii. Others represent unusually large-volume volcanism, whether on plate boundaries, e.g. Iceland, or basalt floods such as the Deccan or Siberian traps.A mantle plume is posited to exist where hot rock nucleates at the core-mantle boundary and rises through the Earth's mantle becoming a diapir in the Earth's crust. The currently active volcanic centers are known as ""hot spots"". In particular, the concept that mantle plumes are fixed relative to one another, and anchored at the core-mantle boundary, was thought to provide a natural explanation for the time-progressive chains of older volcanoes seen extending out from some such hot spots, such as the Hawaiian–Emperor seamount chain.The hypothesis of mantle plumes from depth is not universally accepted as explaining all such volcanism. It has required progressive hypothesis-elaboration leading to variant propositions such as mini-plumes and pulsing plumes. Another hypothesis for unusual volcanic regions is the ""Plate model"". This proposes shallower, passive leakage of magma from the mantle onto the Earth's surface where extension of the lithosphere permits it, attributing most volcanism to plate tectonic processes, with volcanoes far from plate boundaries resulting from intraplate extension.