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ES Ch 3 Test
ES Ch 3 Test

... 11. The hypothesis of _________________________ was that all the continents once were joined as a single supercontinent and have since drifted apart. 12. The process of _________________________ continually adds new crust to the ocean floor along both sides of the mid-ocean ridge. 13. Subduction occ ...
Chapter 8 Plate Tectonics
Chapter 8 Plate Tectonics

... Chapter 8 Plate Tectonics • Plate tectonics ...
Earth and Environmental Science Review with Answers
Earth and Environmental Science Review with Answers

... a. wind power – ADV – cheap DIS – noisy, takes a lot of land b. hydroelectric power – ADV – little pollution, free energy source DIS – dams can get sediment deposits and not work after 50 or so years c. nuclear power – ADV – clean, lots of power DIS – if accident, BIG problems d. solar power – ADV – ...
Mineral resource
Mineral resource

... • Recycled or sold toxic chemical outputs • Began making nonpolluting products • Company saved $1.2 billion • Sparked cleaner production movement ...
No Slide Title - Brookville Local Schools
No Slide Title - Brookville Local Schools

... The layers of the Earth from densest to least dense and how scientists know the makeup of the interior of the Earth ...
Plate tectonics theory
Plate tectonics theory

... PBS, Intro to Plate Tectonic Theory, http://www.pbs.org/wgbh/aso/tryit/tectonics/intro.html, accessed ...
Earthquakes and Volcanoes
Earthquakes and Volcanoes

... pond, these “ripples” are known as seismic waves and these seismic waves are measure using a Richter scale. The Richter Scale was developed by Californian seismologist (a scientist who studies the movements of the Earth), and it allows use to measure the intensity and strength of an earthquake. Seis ...
Landforms provide evidence of change
Landforms provide evidence of change

Lesson
Lesson

... Vortex ...
2.3 Land ppt - Maryville City Schools
2.3 Land ppt - Maryville City Schools

Plate Boundaries and Earthquake Science
Plate Boundaries and Earthquake Science

...  older (some regions up to ~3 billion years old) 2. oceanic crust  thinner (~ 5km)  more dense (gabbroic rocks)  much younger (only up to ~200 million years old) ...
Layers of the Earth Notes The Earth is made of 4
Layers of the Earth Notes The Earth is made of 4

... The Earth's rocky outer crust solidified billions of years ago, soon after the Earth formed. ...
Lecture 3
Lecture 3

... Is a gap created as they move apart? ...
File
File

... Rock itself is a raw material of immense importance. Slates for roofing, ornamental stone for facing buildings, rock chippings for roads, limestone for cement, sand and gravel for aggregate, clays for brick-making and pottery, silica for furnace-linings, gypsum for plaster, rock salt for the dinner ...
Explain briefly what is Geology, it`s branches and it`s importance and
Explain briefly what is Geology, it`s branches and it`s importance and

... divisions of the Time Scale, their time period, and how the divisions were determined.  Define what are fossils and discuss their importance  Explain the age determinations from fossils assemblage.  Explain the half life, parent and daughter isotopes  Describe the different kind of isotopes used ...
HERE
HERE

... • Plate boundaries (convergent and divergent) • SUBDUCTION ZONES: • OCEANIC- CONTINENTAL• As oceanic plate subducts, a deep trench forms. Fluids combine with the crust and mantle and decrease the melting point (this means the rock will melt at a lower temperature);magma rises because less dense than ...
ES Review Packet
ES Review Packet

... __________ The line joining the planet to the Sun sweeps out equal areas in equal times as the planet travels around the ellipse. __________ The ratio of the squares of the revolutionary periods for two planets is equal to the ratio of the cubes of their semimajor axes. __________ The orbits of the ...
Module Title: Code: Level: Credits:
Module Title: Code: Level: Credits:

... Geology for Engineers provides an introduction to several areas of Earth Sciences that impact the engineer, including geological materials, earth surface processes, hydrocarbon exploration and production, natural disasters and climate change. Engineers often need to work with geologists. This module ...
Methods and Equipment Used by Marine Geologists
Methods and Equipment Used by Marine Geologists

... In the 1960's the unifying theory of plate tectonics was proposed to explain many regional and global geologic phenomena, including drifting continents, spreading seafloors, and the worldwide distribution of mountains, earthquakes, and volcanoes. According to the plate tectonic model, the Earth's ou ...
How Rocks are Formed
How Rocks are Formed

... remains a mould. Usually, however, more mineral matter is moved in by water and fills the mould to form a cast. ...
Pacific Northwest
Pacific Northwest

... B. gradually stretch apart and become thinner. C. do not move at all. D. slide sideways without pushing into each other. ...
File
File

... continental drift in________________________. He suggested a supercontinent had existed about 200 million years ago he named________________________________. ...
Ask A Geologist - Miller Museum of Geology
Ask A Geologist - Miller Museum of Geology

... Great question! It sounds like you already know a lot about the moon and how scientists think it formed following a large asteroid impact on the Earth. As a recap, scientists theorize that our solar system itself formed in a big cloud of dust and gases in space called a nebula. In a real simplificat ...
HISTORY OF THE OCEANS
HISTORY OF THE OCEANS

... subduction. Subduction produces earthquakes and volcanoes, also underwater. ...
Name: - Cobb Learning
Name: - Cobb Learning

... 8. Plate Tectonics Theory has been widely accepted since the ___________’s. It states that Earth’s outer layer or _________________ is broken up into ________________. These plates hold ______________________ and _____________________. They are constantly _________________. 9. Continents over time B ...
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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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