Plate Tectonics 10.2
... drift and sea-floor spreading led to the development of a theory called plate tectonics. • Plate tectonics: Theory that Earth's outer shell is divided into several plates that are in motion (glide) over the mantle • Helps explains why and how continents move and is the study of the formation of feat ...
... drift and sea-floor spreading led to the development of a theory called plate tectonics. • Plate tectonics: Theory that Earth's outer shell is divided into several plates that are in motion (glide) over the mantle • Helps explains why and how continents move and is the study of the formation of feat ...
Slide 1
... in any sequence of sedimentary strata, the order in which he strata were deposited from the bottom up. older strata are truncated by erosion before younger strata are deposited. fine deposits overlie coarser units. strata were deposited as horizontal layers. ...
... in any sequence of sedimentary strata, the order in which he strata were deposited from the bottom up. older strata are truncated by erosion before younger strata are deposited. fine deposits overlie coarser units. strata were deposited as horizontal layers. ...
List 1 - arbuthnotbraingame
... solidifying of molten materials. Igneous rocks can form beneath the Earth's surface, or at its surface, as lava. ...
... solidifying of molten materials. Igneous rocks can form beneath the Earth's surface, or at its surface, as lava. ...
File
... Era. Some of the strongest evidence for the theory of plate tectonics emerges from the end of the Paleozoic Era. Geologists think Earth’s land masses formed a single gigantic continent called Pangaea at that time. ...
... Era. Some of the strongest evidence for the theory of plate tectonics emerges from the end of the Paleozoic Era. Geologists think Earth’s land masses formed a single gigantic continent called Pangaea at that time. ...
Types of Plate Boundaries
... are generated as water brought down on the subducting plate melts the overlying mantle, causing magma to rise through the mantle and crust, erupting at the surface. Old crust is destroyed at an oceanic-oceanic boundary. Oceanic-Oceanic Boundary Follow this link and draw the oceanic-oceanic conve ...
... are generated as water brought down on the subducting plate melts the overlying mantle, causing magma to rise through the mantle and crust, erupting at the surface. Old crust is destroyed at an oceanic-oceanic boundary. Oceanic-Oceanic Boundary Follow this link and draw the oceanic-oceanic conve ...
File
... When rock fragments move, they release energy in the form of seismic waves. The point where the earthquake occurs is called the focus. The point on the surface that is directly above the focus is the epicenter. Most earthquakes have a shallow focus because other focuses loose energy before it reache ...
... When rock fragments move, they release energy in the form of seismic waves. The point where the earthquake occurs is called the focus. The point on the surface that is directly above the focus is the epicenter. Most earthquakes have a shallow focus because other focuses loose energy before it reache ...
Plate Tectonics - Department of Physics and Astronomy
... formation of the three major categories of rocks – Igneous Rock ...
... formation of the three major categories of rocks – Igneous Rock ...
Name:______________________________ o ___________________ Samples
... o Plates: a section of the lithosphere that slowly ___________________ over the Asthenosphere ___________________ pieces of the continental and oceanic crust Combined continental drift and sea floor spreading into a ___________________ theory o Scientific Theory: well ___________________ concept t ...
... o Plates: a section of the lithosphere that slowly ___________________ over the Asthenosphere ___________________ pieces of the continental and oceanic crust Combined continental drift and sea floor spreading into a ___________________ theory o Scientific Theory: well ___________________ concept t ...
Review and Study Sheet BRING TO EXAM
... Plate Tectonic Theory of Plate Tectonics Lines of Evidence for Plate Tectonics What is a Hypothesis ? What is a Theory ? What is the Scientific Method ? Chapter 18,19,20 (Plate Tectonics, Seafloor, Continents) What is a plate made of ? Lithosphere Asthenosphere Crust Three types of plate boundaries ...
... Plate Tectonic Theory of Plate Tectonics Lines of Evidence for Plate Tectonics What is a Hypothesis ? What is a Theory ? What is the Scientific Method ? Chapter 18,19,20 (Plate Tectonics, Seafloor, Continents) What is a plate made of ? Lithosphere Asthenosphere Crust Three types of plate boundaries ...
Tectonic Lithospheric Plate Boundaries
... also categorized many different mountains according to their shape. Let’s find out how these shapes came to be. Interact with pages 100 and 101. Use the outline provided to focus your reading. Tectonic Lithospheric Plate Boundaries Convergent – two plates push into each other o Continental/Contine ...
... also categorized many different mountains according to their shape. Let’s find out how these shapes came to be. Interact with pages 100 and 101. Use the outline provided to focus your reading. Tectonic Lithospheric Plate Boundaries Convergent – two plates push into each other o Continental/Contine ...
Week 3 (Norton), part a (pdf, 5.3 MB)
... 4. Note that mountain ranges represent particularly thick continental crust, and beneath those ranges the lithosphere is deformed downward into the asthenosphere (plastic zone). Continental collisions form orogenies because continental crust is too buoyant to be subducted. 5. Standing out in the for ...
... 4. Note that mountain ranges represent particularly thick continental crust, and beneath those ranges the lithosphere is deformed downward into the asthenosphere (plastic zone). Continental collisions form orogenies because continental crust is too buoyant to be subducted. 5. Standing out in the for ...
Plate boundaries - MrD-Home
... volcanoes can form from magma seeping to the surface. • This is how the _____________ volcanic belt of the Pacific Northwest has formed. Coast Mountain Mountain ranges like the ________________ range also form from the collision. _______ Earthquakes can occur when subduction, ridge push and slab pul ...
... volcanoes can form from magma seeping to the surface. • This is how the _____________ volcanic belt of the Pacific Northwest has formed. Coast Mountain Mountain ranges like the ________________ range also form from the collision. _______ Earthquakes can occur when subduction, ridge push and slab pul ...
The Layer`s Of The Earth! - Mrs. V. Murphy`s Science Class
... deformation of the crust as a consequence of plate interaction. ...
... deformation of the crust as a consequence of plate interaction. ...
3. The Earth system
... (1) Divergent boundaries Along divergent boundaries two plates are pulled apart and a large valley forms in between. This is a zone where mantle rock rises toward the Earth’s surface and partially melts. Some of the molten rock (magma) solidifies before reaching the surface. Some reaches the surfa ...
... (1) Divergent boundaries Along divergent boundaries two plates are pulled apart and a large valley forms in between. This is a zone where mantle rock rises toward the Earth’s surface and partially melts. Some of the molten rock (magma) solidifies before reaching the surface. Some reaches the surfa ...
plate tectonics
... – One tectonic plate is forced under another plate as the plates push together. ...
... – One tectonic plate is forced under another plate as the plates push together. ...
F08 4 Igneous
... Magma Igneous rocks are those formed from partially molten (melted) materials Partially molten rock is called magma as it moves through the Earth, and lava when it is extruded at the surface. From where does magma originate? Partial melting of the mantle and crust due to •Influxes of heat •Decreasi ...
... Magma Igneous rocks are those formed from partially molten (melted) materials Partially molten rock is called magma as it moves through the Earth, and lava when it is extruded at the surface. From where does magma originate? Partial melting of the mantle and crust due to •Influxes of heat •Decreasi ...
Inside Earth Unit Study Guide
... 9. What is the driving force of plate movement? 10. What is Pangaea? 11. What are the three types of plate boundaries? 12. List all of the sub-types of plate boundaries and some features of each. 13. Give an example of where each plate boundary occurs. 14. What is paleomagnetism and what does it hav ...
... 9. What is the driving force of plate movement? 10. What is Pangaea? 11. What are the three types of plate boundaries? 12. List all of the sub-types of plate boundaries and some features of each. 13. Give an example of where each plate boundary occurs. 14. What is paleomagnetism and what does it hav ...
Earth`s Interior
... 1. The crust is a layer of rock that forms Earth’s outer skin. There are two types of crust basalt (the crust under the ocean) and granite (the crust under the continents), -Basalt is a dark, dense rock making the oceanic crust. -Granite is a light-colored rock with large crystals making continental ...
... 1. The crust is a layer of rock that forms Earth’s outer skin. There are two types of crust basalt (the crust under the ocean) and granite (the crust under the continents), -Basalt is a dark, dense rock making the oceanic crust. -Granite is a light-colored rock with large crystals making continental ...
Large igneous province
A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.