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Name: India Coghlan. Visit this webpage… http://www.bbc.co.uk
Name: India Coghlan. Visit this webpage… http://www.bbc.co.uk

... Igneous Rocks are formed from Molten rock. Molten rock is called Magma. When magma cools and solidifies, a type of rock called igneous rock forms. Igneous rocks contain crystals rather than grains. The size of the crystal depends on how fast the magma cools. If the magma cools slowly then the crysta ...
The Rock Cycle - Enter Physics Locker
The Rock Cycle - Enter Physics Locker

... conditions. Magma above the Earth’s surface cools quickly, causing only small crystals to form. This is how extrusive igneous rocks like pumice and basalt are made. Magma below the Earth’s surface cools more slowly. There is time for large crystals to grow as the magma solidifies. This is how intrus ...
Igneous rocks
Igneous rocks

... • How are igneous rocks formed? • How does magma differ from lava? • What two criteria are used to classify igneous rocks? • How does the rate of cooling of magma influence the crystal size of minerals in igneous rocks? • How is the mineral makeup of an igneous rock related to Bowen’s reaction serie ...
Document
Document

... Divergent boundary Convergent boundary Subduction zone Transform fault ...
Reviewing Minerals
Reviewing Minerals

... 11. _______________ has a metallic luster. Gypsum’s luster is _______________. 12. Quartz’s luster is _______________. Talc’s is _______________ and Kaolinite’s is _______________. 13. Complete the quiz on the computer program and write the answers below. Pyrite’s luster is _______________. Quartz’ ...
Week 23 Lesson Plan Science 8 all classes
Week 23 Lesson Plan Science 8 all classes

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Terrestrial Worlds in Comparison

... Mercury has signs of ancient volcanic vents. Mars has large, extinct shield volcanoes. ...
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Volacano - OnCourse

... pieces are called bombs (range from a ball to the size of a car). A pyroclastic flow occurs when an explosive eruption hurls out a mixture of hot gases, ash, cinders and bombs. During quiet eruptions, lava flows from vents, setting fire to and then burying ,everything in its path. During an explosiv ...
Subduction Processes in Cascadia
Subduction Processes in Cascadia

... in the form of peat, (undecomposed organic layers) and sand from tsunami deposition. These connections are called peat-mud contacts and peat- sand contacts. They represent a time when the two layers met with some untimely contact. These paleohorizons have been instrumental in developing a reoccuranc ...
What are the characteristics of Earth`s interior?
What are the characteristics of Earth`s interior?

... • Dark, fine rock with fine texture • Continental Crust – Forms the continents – Consists of less dense rocks like granite • Large crystals, not as dense as basalt, light color ...
R7: Taylor-Evolution of Continental Crust
R7: Taylor-Evolution of Continental Crust

... ly useful in deciphering crustal composition because their atoms do not Þt neatly into the crystal structure of most common minerals. They tend instead to be concentrated in the late-forming granitic products of a cooling magma that make up most of the continental crust. Because the REE patterns fou ...
Rocks and the Rock Cycle
Rocks and the Rock Cycle

Rocks and the Rock Cycle
Rocks and the Rock Cycle

... Sedimentary rock can change into metamorphic rock or into igneous rock. Metamorphic rock can change into igneous or sedimentary rock. Almost all of rock today that we have on earth is made up of all the same stuff as the rocks that dinosaurs and other ancient life forms walked, crawled, or swam over ...
Rocks and the Rock Cycle
Rocks and the Rock Cycle

... igneous rock. Metamorphic rock can change into igneous or sedimentary rock. Almost all of rock today that we have on earth is made up of all the same stuff as the rocks that dinosaurs and other ancient life forms walked, crawled, or swam over While the stuff that rocks are made of has stayed the sam ...
The evolution of continental crust
The evolution of continental crust

Types of Magma - Teacher Notes
Types of Magma - Teacher Notes

Types of Magma - Dublin City Schools
Types of Magma - Dublin City Schools

... Andesitic Medium 3-4% Rhyolitic High ...
Chapter 7 earthquakes
Chapter 7 earthquakes

... energy accumulated in rocks. Earthquakes occur when: • Elastic energy exceeds rock strength and the rock breaks forming a fault. • Elastic energy accumulated in the rock exceeds the friction that holds rock along an existing fault line. ...
Plate Tectonics or Does the earth move under your feet?
Plate Tectonics or Does the earth move under your feet?

... 3. Name the four layers of the Earth in order from the outside to the center of the Earth. 4. What causes the mantle to "flow"? 5. What are the two main metals that make up the outer core and the inner core? 6. Describe in your own words how the Earth's ...
Capitanio et al.
Capitanio et al.

... lithosphere is pulled into the mantle, whereas ridge push determines the rate at which the plate is fed to the trench. When slab pull is lowered to values below those of ridge push, as a result of continent entrainment in the mantle, subduction is unable to consume the incoming plate, resulting in t ...
Chapter 5 Key Concepts
Chapter 5 Key Concepts

... belts form along the boundaries of Earth’s plates. Volcanoes can occur where two plates pull apart, or diverge. They can also occur where two plates push together, or converge. The Ring of Fire is one major belt of volcanoes. It includes the many volcanoes that rim the Pacific Ocean. Volcanoes form ...
Chapter 16
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... hardened magma or lava. Source a many non-fuel mineral resources. ...
Magma Supply Vs Magma Plumbing
Magma Supply Vs Magma Plumbing

... • Know the different kinds of earthquakes that occur in subduction zones • Be able to interpret focal mechanisms from subduction zone settings (LAB) ...
Earth
Earth

... The project attempted to drill as deep as possible into the Earth’s crust. Drilling began on 24 May 1970 and in 1989 the hole reached 12 Kilometers (40,230 ft about 7.6miles) and is the deepest hole ever drilled. Drilling ended in 1989 due to lack of funding, which was the same reason why scientists ...
4- Igneous Rock (Intrusive)
4- Igneous Rock (Intrusive)

... Classification of Igneous Rocks Most igneous rocks are classified on the basis of their textures .md composition (~ Figure 4-10). Notice in Figure -I-Ill th.ir all of the rocks, except peridotite, constitute pairs; the members of a pair have the same composition but different textures. Basalt and g ...
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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.
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