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Plate Tectonics and Earth`s Structure
Plate Tectonics and Earth`s Structure

... surface is made up of many plates that move slowly across the mantle. Plate tectonics combines Wegener’s theory of continental drift, seafloor spreading, and other supporting data. Earth’s plates move in different ways and speeds. Although some move faster, most plates move only a few centimeters (o ...
Performance Solid Earth Physics
Performance Solid Earth Physics

... • the gradiometer accelerometers and GPS receiver are based on European technology • the drag free system technology offers new opportunities in a wide range of applications including E.O. from low orbit altitude • a multi-disciplinary user community within fields of Solid Earth Physics, Geodesy and ...
09_test_bank
09_test_bank

... C) a type of metal that tends to create stratovolcanoes when eruptions occur D) a type of mineral that is the main ingredient of sea salt E) another name for lava Answer: B 39) How did the lunar maria form? A) Large impacts fractured the Moon's lithosphere, allowing lava to fill the impact basins. B ...
SGES 1302 Lecture14
SGES 1302 Lecture14

... Once partial melting produces magma, the magma rises towards the Earth surface due to its bouyancy (less dense than the surrounding rocks). A magma’s ability to rise is large controlled by its fluidity (viscosity), which is governed by its temperature and composition. Increasing temperature decrease ...
Metamorphic Rock Lab
Metamorphic Rock Lab

... undergo metamorphism, or changes in structure and mineral content. Elevated temperatures and pressures within the Earth’s crust may cause some or all of the minerals in a pre-existing rock to become unstable and change. Chemically active fluids such as water help to promote changes by adding or subt ...
A geologic cross section is shown below. The most recently formed
A geologic cross section is shown below. The most recently formed

... Which of these events occured most recently at this location? A. ...
Draft Museum Guide - Valley Geology
Draft Museum Guide - Valley Geology

1 the four characteristics of a mineral (Section 1) 2 the two major
1 the four characteristics of a mineral (Section 1) 2 the two major

... the ways that physical features are used to determine relative ages (Section 2) ...
Towards a better understanding of hot spot volcanism
Towards a better understanding of hot spot volcanism

geology of the pacific northwest
geology of the pacific northwest

... The movement of the plates acts a bit like a giant, wide conveyor belt. This conveyor belt is like a flat escalator, used to move people or things across a long space. At divergent boundaries, magma pushes through, cools, and forms new crust. The lithosphere is like a rigid board, though, and as two ...
Term and Lanform - Madison Public Schools
Term and Lanform - Madison Public Schools

... Theory of Plate Tectonics Text pg. 202 - 205 Occurs at midocean ridges. Ridges are at a higher elevation than at the subduction zone. The oceanic lithosphere slides downhill due to the force of gravity as rock cools and becomes more dense. ...
Name: Date: Period:______ ASSIGN PLATE TECTONICS REVIEW
Name: Date: Period:______ ASSIGN PLATE TECTONICS REVIEW

... NOTE: Make sure you explain the significance of the Mariana Trench, Mid-Atlantic Ridge, Iceland, Great Rift Valley, and Himalayas. Mariana Trench: Largest trench in the world. Philippine plate is subducting under the Pacific plate. Is a Oceanic-Oceanic Convergent plate boundary Mid-Atlantic Ridge: L ...
earth science study guide
earth science study guide

... of Earth awesome power that has the potential to wipe out our modern civilization. Will Durant said it best when he wrote “Civilization exist by geological consent, subject to change without notice”. ...
No Slide Title
No Slide Title

... The Geosphere (rock) The Atmosphere (air) The Hydrosphere (water) The Biosphere (living things) ...
Earth`s crust is made up of moving plates.
Earth`s crust is made up of moving plates.

3 The Changing Continents
3 The Changing Continents

... apart. At first, a large rift split Pangaea into two pieces. Scientists call the pieces Laurasia and Gondwanaland. Over time, Laurasia and Gondwanaland also began to break apart. Laurasia broke into pieces that became North America, Europe, and Asia. Gondwanaland broke into pieces that became South ...
Sverdrup Study Guide Ch02 PDF
Sverdrup Study Guide Ch02 PDF

Studi keberadaan logam logam penting (critical metal) dan logam
Studi keberadaan logam logam penting (critical metal) dan logam

... suggesting deposition from REE-bearing groundwater with depleted cerium that results from the element’s insolubility in the oxidized (Ce+4) state. The ore bodies are 3 to 10 m thick and occur mainly in a wholly weathered zone composed of halloysite and kaolinite with residual quartz and feldspar; gr ...
Mantle Processes
Mantle Processes

... One way that mantle peridotites may melt is by plastic flow of large regions toward the surface (i.e., lower pressures). ...
Chapter 13 Notes Worksheet
Chapter 13 Notes Worksheet

Engineering Geology
Engineering Geology

... North America and South America are of this type. Such solutions also percolate through extrusive rock on the ocean floor, forming extensive deposits of metallic sulfides. ...
Magma Formation and Behavior
Magma Formation and Behavior

... • Why are mafic (basaltic) magmas erupted along mid-ocean ridges if they form by the melting of ultramafic rock (peridotite) • Why do granitic (felsic) magmas usually crystallize before reaching Earth’s surface? (Most intrusive rocks are granite) • Why are mafic (basaltic) magmas usually erupted as ...
Inventors and Scientists: Alfred Wegener and Harry Hess
Inventors and Scientists: Alfred Wegener and Harry Hess

... is split down the middle. It belongs to two different plates. The continents have come together into one large mass and then split apart again more than once. Over the last 500 million years, this may have happened as many as three times. The force that moves the plates is thought to be convection c ...
Passing Plates II
Passing Plates II

... The one important finding by scientists about faults is that earthquakes tend to reoccur along faults. This makes sense because faults are areas where the earth's crust is the weakest. There used to be the belief that if stress were relieved on a fault, another earthquake would not occur. In fact, r ...
Chapter 2 - MrJardina
Chapter 2 - MrJardina

... because they are not formed by nature.  Bricks are made from clays and sediments.  Bricks have been used by people for over 60 centuries.  How is the way that bricks are created similar to that of how metamorphic rocks as well as sedimentary rocks are formed? ...
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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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