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Plate Tectonics booklet 19/12/2016 09:30:39 Word Document 550.5
Plate Tectonics booklet 19/12/2016 09:30:39 Word Document 550.5

... Immediate Responses ...
Chapter 9
Chapter 9

... • Lava: magma which reaches the surface of the Earth • Vent: opening in the crust of the Earth where magma is released • Crater: top of a volcano (bowl-shaped) which is connected to the magma chamber by the vent ...
hawaii_vaolcanos
hawaii_vaolcanos

... Mauna Loa with, on its southeast flank, Kilauea and the crater of Halemaumau. Geologically, the islands are young, formed by the underlying plate moving slowly westward over a hot spot in the Earth’s crust, forming a succession of volcanic islands, the oldest island being furthest west and the easte ...
PTOPs Student Information Sheet Answer Key
PTOPs Student Information Sheet Answer Key

... The subduction of the ancient Farallon plate underneath the North American plate caused the uplift of the Sierra Nevadas. Melting of the subducted plate led to the production of magma. ...
Dynamic_Planet_CyFalls_
Dynamic_Planet_CyFalls_

... Magma rising up from the mantle at a divergent boundary Two tectonic plates sliding past one another at a transform boundary Subduction of one oceanic plate under another at a convergent boundary ...
Volcanoes
Volcanoes

... the Earth's Interior b/c of their eruptive history and proximity to major population centers. ...
A Mountain Fact Sheet: Is A Mountain a volcano
A Mountain Fact Sheet: Is A Mountain a volcano

... extended out west towards the Tucson Mountains and into the Tucson Basin (where the city is now). Erosion and faulting are responsible for A Mountain’s place in Tucson and its conical shape. The mountain continues to erode. As volcanoes erupted near A Mountain, around 25 million years ago, they left ...
Plate Tectonics
Plate Tectonics

... • Richter scale – rates earthquakes on times and amplitudes of seismic waves • Moment Magnitude scale – measures amount of energy released – Each number represents 32 x increase in energy ...
Volcano Research Paper
Volcano Research Paper

... Convergent Boundary • A boundary when plates collide and it gets denser and bends • One plate moves under the other (this is called subduction) • As a plate moves down it gets greater heat & pressure • Plates release fluid which causes surrounding rock to melt • When subduction occurs, the denser pl ...
VOLCANIC HAZARDS
VOLCANIC HAZARDS

... The term VOLCANO signifies a vent, hill or mountain from which molten or hot rocks with gaseous materials are ejected. The term also applies to craters, hills or mountains formed by removal of preexisting materials or by accumulation of ejected materials. ...
Day 1 Review - Ms. Canizares
Day 1 Review - Ms. Canizares

... composite volcano ...
Geology Papers Introduction to the Geology of the Mount Shasta
Geology Papers Introduction to the Geology of the Mount Shasta

... sediment that have been folded and faulted into their present positions. To the east stand Mt. Shasta and several lesser peaks of the Cascade range that have been built by flows of lava and ash. As different as these two ranges are, both are the results of the same geologic process: subduction. The ...
AQA A Revision Guide – The Restless Earth
AQA A Revision Guide – The Restless Earth

... ridges to form. Two plates move away from each other. Molten rock (magma) rises from the mantle to fill the gap between the two plates. This forms a mid-ocean ridge. Volcanoes can also form here, along the edges of the plate boundary, due to the rising magma. These volcanoes are called shield volcan ...
Geologic Processes and Features Notes
Geologic Processes and Features Notes

... are usually quiet when they erupt. Hot Spot volcanoes are usually Shield volcanoes. A weak spot in the crust allows these types of volcanoes to form, rather than a plate boundary. __________ ___________ get their name from the material that forms them, cinders. Cinder cones are the simplest volcanic ...
Geology * Part II - Hatboro
Geology * Part II - Hatboro

... change in elevation (stress = shearing) ii. Divergent Boundaries - move apart/may cause a change in elevation (stress = tension) iii. Convergent Boundaries - come together/may cause a change in elevation (stress = compression) ...
Chapter 22 Vocabulary ReviewA Directions: Complete this sheet
Chapter 22 Vocabulary ReviewA Directions: Complete this sheet

... This plate motion creates new sea floor. This happens along the San Andreas fault in California. When two land plates collide, the result is this: Trenches and deep earthquakes occur along this type of plate boundary. ...
Volcanoes
Volcanoes

... A survey of igneous rocks indicates that there are many different types with different chemical compositions. Generally, the composition of igneous rocks can be categorized by the SiO2 content. • Felsic composition rocks are rich in SiO2 and other elements (K and Na). They are generally poor in Fe, ...
Instructions
Instructions

... Volcano: A volcano is created when an opening, or rupture, in a planet's surface or crus! allows hot rnagma, ash and gases to escape from below the surface much like the picture of the volcano to the righf forming in the ocean, off the island of New Zealand. The ash and lava pile up and can produce ...
Nature`s Fury Educator`s Guide - American Museum of Natural History
Nature`s Fury Educator`s Guide - American Museum of Natural History

... the probability of future quakes based on how often they’ve struck a region in the past. Here students can explore the tools scientists use to measure, record, and study Earth’s movements. ...
File
File

... nonexplosive eruptions. • Cinder Cone Volcanoes Cinder cone volcanoes are made of pyroclastic material usually produced from moderately explosive eruptions. • Composite Volcanoes Composite volcanoes, sometimes called stratovolcanoes, are one of the most common types of volcanoes. They form from expl ...
File - Mrs. Ellis` Science Class!
File - Mrs. Ellis` Science Class!

...  Types of pyroclastic debris  Ash and dust - fine, glassy fragments  Pumice - porous rock from “frothy” lava  Cinders - pea-sized material  Lapilli - walnut-sized material  Particles larger than lapilli  Blocks - hardened or cooled lava  Bombs - ejected as hot lava ...
Volcanic Landforms and Processes
Volcanic Landforms and Processes

... Stratovolcanoes • Most active stratovolcanoes on circum-Pacific mountain belt • Associated with subduction zones • Felsic lavas produce explosive eruptions, degassing restricted due to high viscosity • Central part of volcano may explode, or draining of magma chamber and collapse of roof block may c ...
Plate Boundaries
Plate Boundaries

... When the Earth’s magnetic field reverses, the magnetic material in the new rock points toward the new North Pole. As the sea floor spreads away from a mid-ocean ridge, it carries with it a record of magnetic reversals. ...
Constructive Processes
Constructive Processes

... movies/san-andreas1.mov ...
Earth Science Unit - School of Biological Sciences
Earth Science Unit - School of Biological Sciences

... After discovering his grandfather’s invention—the Instant Commuter—twelve-yearold Warren is accidentally transported back in time to Mount St. Helens just moments before its eruption in 1980. A friend Betsy follows him and the two are ...
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Ring of Fire



The Ring of Fire is an area in the basin of the Pacific Ocean where a large number of earthquakes and volcanic eruptions occur. In a 40,000 km (25,000 mi) horseshoe shape, it is associated with a nearly continuous series of oceanic trenches, volcanic arcs, and volcanic belts and/or plate movements. It has 452 volcanoes and is home to over 75% of the world's active and dormant volcanoes. The Ring of Fire is sometimes called the circum-Pacific belt.About 90% of the world's earthquakes and 81% of the world's largest earthquakes occur along the Ring of Fire. The next most seismically active region (5–6% of earthquakes and 17% of the world's largest earthquakes) is the Alpide belt, which extends from Java to the northern Atlantic Ocean via the Himalayas and southern Europe.All but 3 of the world's 25 largest volcanic eruptions of the last 11,700 years occurred at volcanoes in the Ring of Fire.The Ring of Fire is a direct result of plate tectonics and the movement and collisions of lithospheric plates. The eastern section of the ring is the result of the Nazca Plate and the Cocos Plate being subducted beneath the westward moving South American Plate. The Cocos Plate is being subducted beneath the Caribbean Plate, in Central America. A portion of the Pacific Plate along with the small Juan de Fuca Plate are being subducted beneath the North American Plate. Along the northern portion, the northwestward-moving Pacific plate is being subducted beneath the Aleutian Islands arc. Farther west, the Pacific plate is being subducted along the Kamchatka Peninsula arcs on south past Japan. The southern portion is more complex, with a number of smaller tectonic plates in collision with the Pacific plate from the Mariana Islands, the Philippines, Bougainville, Tonga, and New Zealand; this portion excludes Australia, since it lies in the center of its tectonic plate. Indonesia lies between the Ring of Fire along the northeastern islands adjacent to and including New Guinea and the Alpide belt along the south and west from Sumatra, Java, Bali, Flores, and Timor. The famous and very active San Andreas Fault zone of California is a transform fault which offsets a portion of the East Pacific Rise under southwestern United States and Mexico. The motion of the fault generates numerous small earthquakes, at multiple times a day, most of which are too small to be felt. The active Queen Charlotte Fault on the west coast of the Haida Gwaii, British Columbia, Canada, has generated three large earthquakes during the 20th century: a magnitude 7 event in 1929; a magnitude 8.1 in 1949 (Canada's largest recorded earthquake); and a magnitude 7.4 in 1970.
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