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air mass large body of air that has the same characteristics of
air mass large body of air that has the same characteristics of

... area over a long period of time; can be classified by temperature, humidity, precipitation and vegetation ...
Lecture 4
Lecture 4

... Just like in 1543 when Nicolaus Copernicus argued that the planets revolved around the Sun and he was called mad and eccentric, and later when Galileo tried to defend this heliocentric argument, Galileo was tormented and arrested until the day of his death. In the 1960’s geology had a big revolution ...
Science 8 CLASS COPY - DO NOT WRITE ON Ocean Floor Features
Science 8 CLASS COPY - DO NOT WRITE ON Ocean Floor Features

... ocean floor, comprising over 70% of the total sea area. In this domain of darkness, humans have made our most startling discoveries about the earth’s hidden surfaces. The flat sections of the deep-ocean floor turned out to be flatter than anything ever seen on land. Called ​abyssal plains​, these ar ...
METAMORPHISM & METAMORPHIC ROCKS
METAMORPHISM & METAMORPHIC ROCKS

... Deep-sea sediments, those found at depths greater than about 500 m, cover roughly two-thirds of the Earth. The predominant deep sediment is carbonate ooze, which covers nearly half the ocean floor ...
Plate tectonics
Plate tectonics

... NO oceanic plate(s) involved -> Mountain chains ...
1 Mountains and Mountain Ranges
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... Volcanoes erupted and granite plutons formed in the region now called Tibet. ...
Natural Disasters and Sweatshops
Natural Disasters and Sweatshops

... • Out crust of the Earth is made up of a number of shifting tectonic plates that continually bump and slide into each other • In East Asian the Pacific oceanic plate encounters Eurasian continental plate • Leads to building mountains and volcanoes ...
Atlantic Ocean
Atlantic Ocean

...  Over 70,000 kilometers (43,000 miles) in length  Twenty-three percent of Earth’s surface  Winds through all major oceans ...
PLATE TECTONICS - New Jersey City University
PLATE TECTONICS - New Jersey City University

... – Plates move & change in size thru time  Activity at plate boundaries  Combines: – Continental drift – Sea-floor spreading – Paleomagnetism ...
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Overview Plate Tectonics

... 1. During the 1940s and 1950s, scientists began using radar on moving ships to map large areas of the ocean floor in detail. ...
Shorelines - Bakersfield College
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Plate Tectonics - Warren County Public Schools
Plate Tectonics - Warren County Public Schools

... *Break-up of Pangaea occurred around 240 million yrs ago * Over time continents broke up into smaller pieces and have drifted to their current location ...
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List and describe the 3 types of stress
List and describe the 3 types of stress

... What types of land formations are formed at each type of boundary? ...
Plate Tectonics 1
Plate Tectonics 1

...  Prominent lows offshore of arcuate island chains. Note: an ellipse Earth = Equatorial radius about 20 km > polar radius; actual ocean surface (geoid) bulges outward and inward by up to 100 m (highest north of Australia; lowest south of India) ...
The India - Eurasia collision, Himalaya and the Tibetan
The India - Eurasia collision, Himalaya and the Tibetan

... The India - Eurasia collision, Himalaya and the Tibetan plateau. Some important characteristics: • Very long duration of continental collision and shortening • Thickest crust and highest topography on earth ...
The India
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... The India - Eurasia collision, Himalaya and the Tibetan plateau. Some important characteristics: • Very long duration of continental collision and shortening • Thickest crust and highest topography on earth ...
Rocking our world - University of Victoria
Rocking our world - University of Victoria

... This ribbon continent, which Johnston has named SAYBIA (for Siberia, Alaska, Yukon and BC) rested on the Pacific tectonic plate, which slowly moved north, sinking under the Eurasian plate and colliding with Siberia. “As it collided, it buckled like a derailing train,” says Johnston. “The buckled par ...
Volcanoes and Igneous Activity Earth - Chapter 4
Volcanoes and Igneous Activity Earth - Chapter 4

...  Over 70,000 kilometers (43,000 miles) in length  Twenty-three percent of Earth’s surface  Winds through all major oceans ...
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... by a large increase in size of the Earth since its formation. However, this so-called "expanding Earth" hypothesis was unsatisfactory because its supporters could offer no convincing geologic mechanism to produce such a huge, sudden expansion. Most geologists believe that the Earth has changed littl ...
Geological processes in the British Isles
Geological processes in the British Isles

... these continents is recorded by the Caledonian Orogenic Belt, which contains rocks formed within and on the flanks of the now vanished Iapetus (Figure 3d). By ~375 Ma (Figure 3d–e), this ocean had closed with the resultant continental collision producing a series of major tectonic structures that ca ...
Plate Tectonics Section 1 Sea
Plate Tectonics Section 1 Sea

... • In the late 1950s, geologist Harry Hess proposed that the valley at the center of a mid-ocean ridge was a crack, or rift, in Earth’s crust. • As the ocean floor moves away from the ridge, molten rock, or magma, rises to fill the crack. • sea-floor spreading the process by which new oceanic lithosp ...
In geologic terms, a plate is a large, rigid slab of solid rock
In geologic terms, a plate is a large, rigid slab of solid rock

... Alfred Wegener. He contended that, around 200 million years ago, the supercontinent Pangaea, meaning “all lands” or “all Earth”, began to split apart. At first it was proposed that Pangaea first broke into two large continental landmasses, Laurasia in the northern hemisphere and Gondwanaland in the ...
Year 8: Tectonics: Revision worksheet SS2017 1. Constructive plate
Year 8: Tectonics: Revision worksheet SS2017 1. Constructive plate

... Emergency bin (and water) Deep foundations ...
Chapter 11: The Archean Eon of Precambrian Time
Chapter 11: The Archean Eon of Precambrian Time

... – orogenies weld large continental masses together ...
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Pangaea



Pangaea or Pangea (/pænˈdʒiːə/) was a supercontinent that existed during the late Paleozoic and early Mesozoic eras. It assembled from earlier continental units approximately 300 million years ago, and it began to break apart about 175 million years ago. In contrast to the present Earth and its distribution of continental mass, much of Pangaea was in the southern hemisphere and surrounded by a super ocean, Panthalassa. Pangaea was the last supercontinent to have existed and the first to be reconstructed by geologists.
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