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Planet Earth - Wayne State University Physics and Astronomy
Planet Earth - Wayne State University Physics and Astronomy

... A fourth kind of rock is primitive rock Its formation is believed to date back to the formation of the planet Primitive rock has largely escaped chemical modification by heating Thus, it is thought to represent the original material out of which the planetary system was made No primitive rock is lef ...
Chapter_14_Notes
Chapter_14_Notes

... b) The solution drains into storage ponds below the rocks c) After circulated a number of times, the gold is removed from the ponds 3) Cyanide is extremely toxic to birds and mammals 4) Cyanide can leak into underground drinking water supplies and poison fish and other forms of life in lakes and str ...
File - Mr. Catt`s Class
File - Mr. Catt`s Class

... 1. The period of the Moon’s rotation exactly matches its period of revolution. This is caused by tidal forces, and as a result the Moon keeps the same face toward Earth at all times. 2. There are frictional forces between the solid Earth and its oceans. The Earth’s motion tends to drag the tides alo ...
EarthHW_Eqk_Vol
EarthHW_Eqk_Vol

... It will move faster and faster because there is no force to stop it. It will stop gradually because there is no force to keep it moving. It will stop immediately when the force that started its motion has stopped. Its motion will not change, and it will continue in the same direction at the same ...
The Oldest Rocks on Earth
The Oldest Rocks on Earth

... quartzite. That, Mojzsis decided, offered a way to test whether the Nuvvuagittuq rocks were the oldest on the planet. Geologists have seen similar arrangements in much younger formations. They occur when underwater volcanoes spread molten rock across the ocean floor. Sometimes the volcanoes die down ...
Precambrian Era PPT 2
Precambrian Era PPT 2

... looked like modern jellyfish and worms  Stromatolites: layered mats formed by colonies or groups of cyanobacteria (blue-green algae thought to be the first or one of the earliest life forms on Earth.)  Invertebrates (animals with no backbone) appeared near the end of the Precambrian ...
280 something ways
280 something ways

... In inferences are conclusions or predictions based on your observations. Ex: The rock is old. Your senses can be extended (made more precise) by using instruments. Ex: The book is 22cm. Classification is organizing observations in a meaningful way. Ex: The book is science fiction. Mass- the amount o ...
Plate Tectonics
Plate Tectonics

... body wave is a seismic wave that moves through the interior of the earth, as opposed to surface waves that travel near the earth's surface. P and S waves are body waves. Each type of wave shakes the ground in different ways. ...
Plate Tectonic Overview and Introduction to Energy, Work, and Heat
Plate Tectonic Overview and Introduction to Energy, Work, and Heat

... Rock densities range from 2.7 (crust) to 3.3 g/cm3 (mantle) 270 bar/km for the crust and 330 bar/km for the mantle ...
Earth Structure
Earth Structure

... Rock densities range from 2.7 (crust) to 3.3 g/cm3 (mantle) 270 bar/km for the crust and 330 bar/km for the mantle ...
Earth as a System - Bakersfield College
Earth as a System - Bakersfield College

... 1. Explain why the scientific method is a useful tool for learning about the processes that occur in our universe. 2 Define the steps within the scientific method. I will get an A on my exams and quizzes. ...


... Metamorphic rocks are the only rocks that forms directly from other rocks whose original form has been altered by heat, pressure or chemically active fluids. This alteration of rocks is called RECRYSTALLIZATION . ...
File
File

... • From seismic and other geophysical evidence and laboratory experiments, scientists agree with the theory that the plate-driving force is the slow movement of hot, softened mantle that lies below the rigid plates • Below the lithospheric plates, at some depth the mantle is partially molten and can ...
What is Geology?
What is Geology?

... plates of the lithosphere to move. Heated material in the asthenosphere becomes less dense and rises toward the solid lithosphere, through which it cannot rise further. It therefore begins to move horizontally, dragging the lithosphere along with it and pushing forward the cooler, denser material in ...
282 WAYS TO PASS THE EARTH SCIENCE REGENTS
282 WAYS TO PASS THE EARTH SCIENCE REGENTS

... In inferences are conclusions or predictions based on your observations. Ex: The rock is old. Your senses can be extended (made more precise) by using instruments. Ex: The book is 22cm. Classification is organizing observations in a meaningful way. Ex: The book is science fiction. Mass- the amount o ...
282 Ways to Pass Earth Science Regents
282 Ways to Pass Earth Science Regents

... In inferences are conclusions or predictions based on your observations. Ex: The rock is old. Your senses can be extended (made more precise) by using instruments. Ex: The book is 22cm. Classification is organizing observations in a meaningful way. Ex: The book is science fiction. Mass- the amount o ...
1 Billion Years Ago 450 Million Years Ago 400 Million Years Ago
1 Billion Years Ago 450 Million Years Ago 400 Million Years Ago

... standing near a soaring mountain range on a giant continent called Pangea. The rocks you see today were formed on the floor of an ancient ocean that divided that continent as plates in the Earth’s crust moved apart. Today’s Green Mountains formed as these plates eventually collided again, closing th ...
The Layers of Earth
The Layers of Earth

... crust and mantle rose to the surface, separating into layers around the innermost, dense core. 4 As one travels down through Earth's layers, there are increases in both temperature and pressure, which are due to the mass of the overlying layers of rock. The mantle is the second layer of Earth. The u ...
Weathering PPT
Weathering PPT

... Process that breaks down and changes rock at or near earth’s surface ...
geology
geology

... standing near a soaring mountain range on a giant continent called Pangea. The rocks you see today were formed on the floor of an ancient ocean that divided that continent as plates in the Earth’s crust moved apart. Today’s Green Mountains formed as these plates eventually collided again, closing th ...
2.0 The Rock Cycle describes how rocks form and change over time
2.0 The Rock Cycle describes how rocks form and change over time

... -shale (formed from fine clay or mud) -sandstone (sand, made of quartz) -conglomerate (pebbles and small stones cemented together) -limestone (organic sedimentary rock, containing fossils - plant and animal remains) -organic sedimentary rock forms from living material that has been buried and is und ...
Chapter 10 Section 3
Chapter 10 Section 3

... mantle that transfers heat in Earth's interior and is the driving force for plate tectonics. It is also known as the cycle of heating, rising, and cooling. ...
Science Review Checklist5
Science Review Checklist5

... 89. What part of the cell stores food, water, and waste? 90. What part of the cell is a jelly-like substance that contains ...
Plate Tectonics
Plate Tectonics

...  Heat is transferred in the mantle through radiation, conduction, and convection.  Radiation is the transfer of heat through empty space.  Conduction is heat transfer by direct contact of particles of matter.  Convection is heat transfer by the movement of heated liquid. ...
Chapter 7 - Earth and the Terrestrial Worlds
Chapter 7 - Earth and the Terrestrial Worlds

... after the solar system formed (“Period of Heavy Bombardment”). ...
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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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