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chpt 17 continental drift
chpt 17 continental drift

... plates move past each other. The plates do not have smooth edges so there is tremendous friction that keeps them from sliding...until enough pressure builds up, and then the plates move suddenly. This sudden movement is what we call an earthquake.  The boundary where the two plates move past each o ...
GE 121 Physical and Historical Geology I Earth’s Dynamic Systems 10
GE 121 Physical and Historical Geology I Earth’s Dynamic Systems 10

... relations, (d) inclusions, and (e) succession in landscape development. 3. The standard geologic column was established from studies of rock sequences in Europe. It is now used worldwide. Rocks were originally correlated from different parts of the world largely based on the fossils they contain. To ...
History of the Earth Chapter 2: The Hadean
History of the Earth Chapter 2: The Hadean

... Basic Plate Tectonics • Earth’s “surface” (lithosphere) is broken into plates • Plates move on asthenosphere • “Geology happens” where the plates interact with one another ...
Geol 101: Physical Geology Spring 2002
Geol 101: Physical Geology Spring 2002

... B. Earth’s magnetic field reverses about every half million years C. plate tectonics causes continents and ocean crust to slowly drift away from ridges D. new ocean crust is constantly being created at mid-ocean ridges E. all of the above 19. The oldest oceanic crust beneath the ocean basins occurs: ...
Earth and Space Science Objective Booklet 4a. Compare and
Earth and Space Science Objective Booklet 4a. Compare and

... 5) What is a plate and what is the theory of plate tectonics? What forces drive the movement of tectonic plates? 6) What occurs at divergent plate boundaries and what do they form? 7) What occurs at convergent plate boundaries and what do they form? (Oceanic/Continental, Continental/ Continental, Oc ...
CAUSES OF CHANGE: GEOLOGICAL EVOLUTION
CAUSES OF CHANGE: GEOLOGICAL EVOLUTION

... • First theory to describe Earth’s mountain ranges was better known as “dried Apple theory”- stated that as the Earth’s surface cooled it did so at unequal rates causes parts to collapse and created mountains. • Commonly believed until Alfred Wegner challenged it with his idea of Continental Drift ( ...
THE INCREDIBLE EDIBLE EARTH LAB
THE INCREDIBLE EDIBLE EARTH LAB

... 2. Is this what would happen if someone took a giant knife and cut the Earth’s crust? ____________________ Why or why not? _______________________________________________________________ ____________________________________________________________________________ 3. What is the thickest measure of t ...
PlateTec1617 - Biloxi Public Schools
PlateTec1617 - Biloxi Public Schools

... plate located beneath a plate remains in one place as plate above it moves creates chain of small volcanoes no longer active when not over the hot spot Hawaiian Islands--different ages of islands a wave of energy that travels away from the center of an earthquake in all directions increase going int ...
Plate Tectonics and Continental Drift
Plate Tectonics and Continental Drift

... • Plates are active participants in the convection process – Slab pull – dense ocean crust descends under its own weight – Ridge push – gravity pulls lithosphere down & away from ridge – Friction – resistance to movement from various sources ...
Our Changing Earth: Plate Tectonics and Large
Our Changing Earth: Plate Tectonics and Large

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Exogenous Forces and Weathering
Exogenous Forces and Weathering

... both break up and decompose. What causes these two processes of weathering? The breaking up occurs by means of physical weathering. The decomposition occurs by means of chemical weathering. Rock exposed to these two processes changes size and shape. It is then transported by gravity, water, wind, an ...
We will study the structure and
We will study the structure and

Chlorine cycling during subduction of altered oceanic crust
Chlorine cycling during subduction of altered oceanic crust

... Understanding the exchange of volatiles between the mantle and the exosphere, including their accumulation in surface reservoirs via outgassing of the Earth's interior, the degree of mantle depletion and the extent of recycling back into the mantle, represents a central issue of terrestrial geodynam ...
Chapter6
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... 3. According to the fission hypothesis, the large basin of the Pacific Ocean is the place from which the Moon was ejected. This theory cannot explain the Moon’s current orbit nor offer an adequate rationale for what force could have caused the Moon to be torn from the Earth. 4. According to the capt ...
benefits of geodetic techniques on earthquake researches
benefits of geodetic techniques on earthquake researches

I. Earth spheres A. Three major spheres 1. atmosphere, thin
I. Earth spheres A. Three major spheres 1. atmosphere, thin

... responsible for reactions with other atoms b) full shells are not reactive i. first shell can contain 2 electrons ii. successive outer shells can contain 8 electrons c. atom is electrically neutral when it has the same number of electrons and protons VI. Periodic table of elements A. Each atom is re ...
Name: 1 GEOL 104 Dinosaurs: A Natural History Geology
Name: 1 GEOL 104 Dinosaurs: A Natural History Geology

... and its fossils are found both in North America and eastern Asia. Fossils of Amia remain nearly identical throughout the last 95 million years. ...
Warm-Up - mssarnelli
Warm-Up - mssarnelli

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Rocks
Rocks

... 1. How does an igneous rock change into a sedimentary rock?  2. How does a sedimentary rock change into a metamorphic rock?  3. How does a metamorphic rock change into an igneous rock?  4. What is an index mineral?  5. How are metamorphic rocks classified? ...
Continental Drift Powerpoint
Continental Drift Powerpoint

... In 1912, a German scientist (he was an explorer, astronomer, and meteorologist) proposed that at one time all of the continents had been joined together to form one huge continent  His name was Alfred Wegener  He called this supercontinent Pangaea (it means “all Earth”)  And, over time (millions ...
Origin of magma (pg.270-273)
Origin of magma (pg.270-273)

... 3. Decompression melting of rock occurs when rocks (ascend, descend)? Explain. 4. What effect do volatiles (such as water) have on the melting temperature of rock? 5. Do all minerals melt at the same temperature? Explain the partial melting of magma? ...
שקופית 1
שקופית 1

... or: Any mass of mineral matter which forms part of the Earth’s crust. Rock may consist of only one mineral species (mono-mineral rock) or be an aggregate of mineral species. ...
Lesson 2 | Shaping Earth`s Surface
Lesson 2 | Shaping Earth`s Surface

... Directions: On the line before each statement, write T if the statement is associated with transform boundaries, D if the statement is associated with divergent boundaries, or C if the statement is associated with convergent boundaries. ...
The Ever-Changing Surface of the Earth
The Ever-Changing Surface of the Earth

... decomposition of rocks, minerals, and immature soils at or near the Earth's surface. Weathering also initiates the erosion of rock, causing changes in the surface layers of the Earth. ...
Rocks and Minerals posted version
Rocks and Minerals posted version

... —Last minerals - higher amounts of silica and lower melting point ...
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Age of the Earth



The age of the Earth is 4.54 ± 0.05 billion years (4.54 × 109 years ± 1%). This age is based on evidence from radiometric age dating of meteorite material and is consistent with the radiometric ages of the oldest-known terrestrial and lunar samples.Following the development of radiometric age dating in the early 20th century, measurements of lead in uranium-rich minerals showed that some were in excess of a billion years old.The oldest such minerals analyzed to date—small crystals of zircon from the Jack Hills of Western Australia—are at least 4.404 billion years old. Comparing the mass and luminosity of the Sun to those of other stars, it appears that the Solar System cannot be much older than those rocks. Calcium-aluminium-rich inclusions – the oldest known solid constituents within meteorites that are formed within the Solar System – are 4.567 billion years old, giving an age for the solar system and an upper limit for the age of Earth.It is hypothesised that the accretion of Earth began soon after the formation of the calcium-aluminium-rich inclusions and the meteorites. Because the exact amount of time this accretion process took is not yet known, and the predictions from different accretion models range from a few millions up to about 100 million years, the exact age of Earth is difficult to determine. It is also difficult to determine the exact age of the oldest rocks on Earth, exposed at the surface, as they are aggregates of minerals of possibly different ages.
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