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GEO144_final_key
GEO144_final_key

... C) shield volcanoes are constructed with lava with higher percent Si and hotter temperatures D) shield volcanoes are constructed with lava with lower percent Si and hotter temperatures (67) 1 pt. Which rocks are sorted properly, from low Si to high Si content? A) Rhyolite, Dacite, Andesite, Basalt B ...
Minerals and Rocks
Minerals and Rocks

... where many volcanoes erupt lava of this composition) represent this intermediate composition (see again Fig. 13.11). Many igneous rocks are broken along fractures that may be spaced or arranged in regular geometric patterns. In the Earth sci- ...
File - Vagabond Geology
File - Vagabond Geology

... But first a word about the earth’s crust Oceanic Crust: Under all of the deep seas About 5 miles thick Continental Crust: Comprises all continents About 20 to 50 miles thick ...
Inosilicates (Pyroxenes and Amphiboles)
Inosilicates (Pyroxenes and Amphiboles)

... Hornblende - is a common mineral in both igneous and metamorphic rocks. In igneous rocks it is found in andesites, dacites, and rhyolites, as well as in gabbros, diorites, and granites. In metamorphic rocks it is a common constituent of meta-basalts that have been metamorphosed to intermediate grade ...
Geological slant on plates
Geological slant on plates

... and Africa. It seems very unlikely either that they could have crossed thousands of miles of ocean or evolved identically on separate continents. • Fossils of Glossopteris, a seed fern, from 270Ma are found across the southern continents. • Coal is found in Antarctica; coal is unlikely to have forme ...
Plate Tectonic, Earthquakes, and Volcanoes Test Review
Plate Tectonic, Earthquakes, and Volcanoes Test Review

... 11. The (newest/ oldest) crust is farthest away from the mid-ocean ridges. 12. How do oceanic magnetic stripes provide proof of sea floor spreading? When new oceanic crust is still molten, the magnetic grains will align with the magnetic poles (like a compass). Throughout Earth’s history, the poles ...
if they
if they

Chapter 1 Introduction – Review of Rocks and
Chapter 1 Introduction – Review of Rocks and

... exhibit a black to dark gray color (Figure 4).   Of the sum of quartz, plagioclase, and K‐feldspar, a  gabbro or diorite would be composed of 90% ‐ 100% plagioclase, 0% ‐ 10% K‐feldspar, and 0% ‐  5% quartz (Figures 2 and 4).  In addition, the dark colored minerals olivine, amphibole, and/or  ...
oceanic ridges
oceanic ridges

... Another subduction zone—this one with oceanic material on both sides. O-O Modern example of volcanic islands: Japan ...
Plate Tectonics 1
Plate Tectonics 1

... and solid layer broken into plates that move •Oceanic crust is mostly basalt •Continental crust is composed of granite ...
Volcanism and Volcanoes
Volcanism and Volcanoes

... fine sediment (mud and clay) that either (1) pours gently from a vent in the ground like a fluid lava flow; or (2) is ejected into the air like a lava fountain by escaping volcanic gas and boiling water. ...
4 Igneous Rocks - North Coast Distance Education
4 Igneous Rocks - North Coast Distance Education

... Basaltic magmas produce rocks of the gabbro-basalt family, which are composed of Ca-plagioclase and pyroxene with lesser amounts of olivine and little or no quartz. Magmas with composition intermediate between mafic and silicic compositions produce rocks of the diorite-andesite family. Basalt, the m ...
Chapter 2 - Mineral and Rocks
Chapter 2 - Mineral and Rocks

... – sawed and polished rocks for tombstones, monuments, mantle pieces and counter tops – Even the soils we depend on • for most of our food • formed by alteration of rocks ...
No Slide Title
No Slide Title

... Narrowly Defined Chemical Composition • Some minerals have very specific compositions – examples are halite (NaCl) or quartz (SiO2) ...
Intrusive and Extrusive Igneous Rocks - cK-12
Intrusive and Extrusive Igneous Rocks - cK-12

... Intrusive igneous rocks cool underground. Deep in the crust, magma cools slowly. Slow cooling gives crystals a chance to grow. Intrusive igneous rocks have relatively large crystals that are easy to see. Intrusive igneous rocks are also called plutonic. A pluton is an igneous rock body that forms wi ...
Convergent boundary
Convergent boundary

Rock Cycle - pcmmsmiller
Rock Cycle - pcmmsmiller

... Formation of Sedimentary Rocks • Two main groups of sedimentary rocks – Clastic rocks: made of sediments that were weathered, transported, and deposited in layers – Chemical rocks: formed from minerals that were dissolved in water, came out of solution, and deposited ...
Chapter Excerpt
Chapter Excerpt

... vent or opening in the crater and flows freely out over the earth’s surface until it cools and hardens into a layer of igneous rock. Repeated lava flows builds this type of volcanoe into the largest volcanic mountain. Mauna Loa found in Hawaii, is the largest volcano on earth. Cinder Cone Volcanoes ...
Plate Tectonics and Continental Drift
Plate Tectonics and Continental Drift

... 1. What are the theories of Plate Tectonics and Continental Drift? 2. What is the evidence that Continents move? 3. What are the forces that drive plate tectonics? 4. What happens at the boundaries between plates? 5. How do the different types of plate boundaries impact the regional geology and geom ...
Intrusive and Extrusive Igneous Rocks
Intrusive and Extrusive Igneous Rocks

... Intrusive igneous rocks cool underground. Deep in the crust, magma cools slowly. Slow cooling gives crystals a chance to grow. Intrusive igneous rocks have relatively large crystals that are easy to see. Intrusive igneous rocks are also called plutonic. A pluton is an igneous rock body that forms wi ...
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 ...
Metamorphism and Metamorphic Rocks
Metamorphism and Metamorphic Rocks

... Transition of one rock into another by temperatures and/or pressures unlike those in which it formed Metamorphic rocks are produced from •Igneous rocks •Sedimentary rocks •Other metamorphic rocks Metamorphism progresses incrementally from low-grade to high-grade During metamorphism the rock must ...
Eclogite formation and the rheology, buoyancy, seismicity, and H2O
Eclogite formation and the rheology, buoyancy, seismicity, and H2O

... Mid-ocean-ridge basalts(MORBs) typicallyareglassy or containplagioclasewith lessolivine [Hekinian,1982], while rockscrystallizedin intraoceanicmagmaticarcsgenerally containplagioclaseand augite [Ewart, 1982]. Midocean-ridgebasalts (MORBs) are subalkalinetholeiites that typically contain plagioclase ...
Chapter 9
Chapter 9

The Ever-Changing Surface of the Earth
The Ever-Changing Surface of the Earth

... them to other locations. These rocky materials are transported after the process of weathering has broken bedrock down into smaller, moveable pieces. The primary agents of weathering are water, ice, and gases in the atmosphere. Although weathering and erosion often occur at the same time, they are n ...
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Basalt



Basalt (pronounced /bəˈsɔːlt/, /ˈbæsɒlt/, /ˈbæsɔːlt/, or /ˈbeɪsɔːlt/)is a common extrusive igneous (volcanic) rock formed from the rapid cooling of basaltic lava exposed at or very near the surface of a planet or moon. Flood basalt describes the formation in a series of lava basalt flows.
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