Rocks - easternlocal.com
... Have your rock graphic organizer out and fill it in as the video goes on. We will discuss it at the end of the video. ...
... Have your rock graphic organizer out and fill it in as the video goes on. We will discuss it at the end of the video. ...
Topic 12 guided reading answer key
... 36. What features other than lava flows are associated with divergent boundaries? VOLCANOES, EARTHQUAKES, RIFT VALLEYS 37. When divergence is within the oceanic crust, the faulting and volcanic activity result in a MID-OCEAN RIDGE, a mountain range at the bottom of the ocean that is composed mostly ...
... 36. What features other than lava flows are associated with divergent boundaries? VOLCANOES, EARTHQUAKES, RIFT VALLEYS 37. When divergence is within the oceanic crust, the faulting and volcanic activity result in a MID-OCEAN RIDGE, a mountain range at the bottom of the ocean that is composed mostly ...
Rocks - Fort Thomas Independent Schools
... o Foliated -- aligned sheet or plate-like layered structure (gneiss and schist) o Non-foliated – non aligned layers (marble and slate) ...
... o Foliated -- aligned sheet or plate-like layered structure (gneiss and schist) o Non-foliated – non aligned layers (marble and slate) ...
Rocks - Fort Thomas Independent Schools
... • Classified based on texture • Foliated -- aligned sheet or plate-like layered structure (gneiss and schist) • Non-foliated – non aligned layers (marble and slate) ...
... • Classified based on texture • Foliated -- aligned sheet or plate-like layered structure (gneiss and schist) • Non-foliated – non aligned layers (marble and slate) ...
Chapter 17: Plate Tectonics
... 2. Oceanic crust a) is almost completely basalt b) very dense c) always sinks underneath continental crust D. Hot Spot 1. An area in the middle of the crust with a high heat flow a) magma is rising upward through the crust 2. Causes volcanoes and volcanic islands to form a) Ex. Hawaii 3. The hot spo ...
... 2. Oceanic crust a) is almost completely basalt b) very dense c) always sinks underneath continental crust D. Hot Spot 1. An area in the middle of the crust with a high heat flow a) magma is rising upward through the crust 2. Causes volcanoes and volcanic islands to form a) Ex. Hawaii 3. The hot spo ...
Study Guide 9 -
... An enormously varied amount of data has accumulated in support of the theory of plate tectonics. a. The mid-oceanic ridges represent sites of the creation of seafloor. (see p.180-181) b. The record of paleomagnetism preserved in seafloor rocks reveals a pattern of seafloor spreading away from mid-oc ...
... An enormously varied amount of data has accumulated in support of the theory of plate tectonics. a. The mid-oceanic ridges represent sites of the creation of seafloor. (see p.180-181) b. The record of paleomagnetism preserved in seafloor rocks reveals a pattern of seafloor spreading away from mid-oc ...
Chapter 17 - Auburn City Schools
... Describe one piece of early evidence that led people to suggest the Earth’s continents my ...
... Describe one piece of early evidence that led people to suggest the Earth’s continents my ...
Chapter 1 Study Guide – Plate Tectonics
... Bonus Question: What were the 3 types of evidence that supported Hess’s theory of sea floor spreading? a. eruptions of molten material b. magnetic stripes in the rock of the ocean floor c. the ages of the rocks ...
... Bonus Question: What were the 3 types of evidence that supported Hess’s theory of sea floor spreading? a. eruptions of molten material b. magnetic stripes in the rock of the ocean floor c. the ages of the rocks ...
5. North Atlantic Tertiary Igneous Province (NATP)
... 5. Igneous material was also injected into the country rocks as dykes. Often they were so numerous as to occur in what are called dyke swarms 6. 55 mya continental rifting over hot spot & ocean-floor spreading started & North Atlantic opened 7. 50 mya a constructive plate margin developed & can now ...
... 5. Igneous material was also injected into the country rocks as dykes. Often they were so numerous as to occur in what are called dyke swarms 6. 55 mya continental rifting over hot spot & ocean-floor spreading started & North Atlantic opened 7. 50 mya a constructive plate margin developed & can now ...
Chapter 6-Study Questions
... ___14. Synclines are upfolded rock layers that form from the bending of previously flat-lying sedimentary and volcanic rocks. ___15. Most major mountain ranges form along convergent plate boundaries. ___16. Most of the motions that produce earthquakes can be satisfactorily explained by the plate te ...
... ___14. Synclines are upfolded rock layers that form from the bending of previously flat-lying sedimentary and volcanic rocks. ___15. Most major mountain ranges form along convergent plate boundaries. ___16. Most of the motions that produce earthquakes can be satisfactorily explained by the plate te ...
Plate Tectonics Notes 2015-2016
... a wave of energy that travels away from the center of an earthquake in all directions increase going into Earth because they are moving from less dense material to more dense material most common where plates slide by each other fault--- break, or crack, in Earth’s surface along ...
... a wave of energy that travels away from the center of an earthquake in all directions increase going into Earth because they are moving from less dense material to more dense material most common where plates slide by each other fault--- break, or crack, in Earth’s surface along ...
Document
... 3. Why do less dense compounds make up Earth’s crust while the densest compounds make up the core? _______________________________________________________________ _______________________________________________________________ 4. List the three layers of the Earth, based on their chemical compositio ...
... 3. Why do less dense compounds make up Earth’s crust while the densest compounds make up the core? _______________________________________________________________ _______________________________________________________________ 4. List the three layers of the Earth, based on their chemical compositio ...
01 - Mayfield City Schools
... 3. Why do less dense compounds make up Earth’s crust while the densest compounds make up the core? _______________________________________________________________ _______________________________________________________________ 4. List the three layers of the Earth, based on their chemical compositio ...
... 3. Why do less dense compounds make up Earth’s crust while the densest compounds make up the core? _______________________________________________________________ _______________________________________________________________ 4. List the three layers of the Earth, based on their chemical compositio ...
directed reading inside earth
... 3. Why do less dense compounds make up Earth’s crust while the densest compounds make up the core? _______________________________________________________________ _______________________________________________________________ 4. List the three layers of the Earth, based on their chemical compositio ...
... 3. Why do less dense compounds make up Earth’s crust while the densest compounds make up the core? _______________________________________________________________ _______________________________________________________________ 4. List the three layers of the Earth, based on their chemical compositio ...
Geo 1-2 Tectonic Plates Notes
... Plate Tectonics • Theory that earth’s outer shell (crust) is not one solid sheet of rock…more like a jigsaw puzzle • Each plate moves separately – Movements can lead to earthquakes, volcanoes and more ...
... Plate Tectonics • Theory that earth’s outer shell (crust) is not one solid sheet of rock…more like a jigsaw puzzle • Each plate moves separately – Movements can lead to earthquakes, volcanoes and more ...
Don`t Break Your Plate
... Crust is destroyed and recycled back into the Earth’s interior as one plate sinks below another plate— subduction zones ...
... Crust is destroyed and recycled back into the Earth’s interior as one plate sinks below another plate— subduction zones ...
Alfred Wegener was a scientist who lived about 100 years ago
... system of cracks on the sea-floor called mid-ocean ridges. Another new technology called radioactive dating allowed scientists to measure the age of rocks. They discovered that the sea floor near mid-ocean ridges is very young while rocks farther away are much older. These discoveries led to the ide ...
... system of cracks on the sea-floor called mid-ocean ridges. Another new technology called radioactive dating allowed scientists to measure the age of rocks. They discovered that the sea floor near mid-ocean ridges is very young while rocks farther away are much older. These discoveries led to the ide ...
History of the Earth Chapter 2: The Hadean
... “If we are to believe Wegener’s Hypothesis, we must forget everything which has been learned in the last 70 years and start over again.” –Critic of Continental Drift in ...
... “If we are to believe Wegener’s Hypothesis, we must forget everything which has been learned in the last 70 years and start over again.” –Critic of Continental Drift in ...
Plate Tectonics Review Worksheet
... 6. What is the lithosphere – Solid outer layer of the earth that consists of the crust and the rigid upper portion of the mantle. What is the Asthenosphere - the soft layer of the mantle on which the tectonic plates move. What is the Mesosphere – the strong lower part of the mantle between the asthe ...
... 6. What is the lithosphere – Solid outer layer of the earth that consists of the crust and the rigid upper portion of the mantle. What is the Asthenosphere - the soft layer of the mantle on which the tectonic plates move. What is the Mesosphere – the strong lower part of the mantle between the asthe ...
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.