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Powerpoint Presentation Physical Geology, 10th ed.
Powerpoint Presentation Physical Geology, 10th ed.

... • Top of a plate – consisting of oceanic crust, continental crust or a part of each • North American Plate is moving westward relative to Europe – Plate’s divergent boundary is along midoceanic ridge in the North Atlantic Ocean • Transform Boundary: San Andreas Fault in CA is an example – Earthquake ...
Unit 1 Goal 1: Unique Planet
Unit 1 Goal 1: Unique Planet

... (gravity) between two objects depends on their masses and the distance between them. The more massive they are and the closer they are together, the greater the attraction. Mass is the amount of matter that makes up an object. Weight is the effect of gravity on that mass. The father you are from the ...
1 - Blinklearning
1 - Blinklearning

5.1 notes What processes change Earth`s crust? Objective: Compare
5.1 notes What processes change Earth`s crust? Objective: Compare

... Some changes in Earth’s surface occur very suddenly. Some take hundreds, thousands even millions of years to happen. Over time, pressure in Earth’s crust can cause layers to bend, curve, or wrinkle. This is called Folding. Rocks may crack underneath, but the layers stay together. Upward folds are ca ...
57. Practice reading seismographs: Can You Read a Quake?
57. Practice reading seismographs: Can You Read a Quake?

... 46. Describe paleomagnetism. How is the study of paleomagnetism used in Earth science? The study of the alignment of magnetic materials in rocks, especially to understand and describe the reversal of Earth’s magnetic poles. Used in Earth science to support the theory of sea floor spreading and the t ...
OAA prep-
OAA prep-

... Mitosis produces daughter cells that are genetically identical to the parent cell; Meiosis produces sex cells containing half the genetic material of the parent cell; Sexual reproduction involves the combining of sex cells, which results in an organism with genetic material from the parent(s); Asexu ...
Notes Chapter 28
Notes Chapter 28

... Over geologic history, many animals and plants have lived and become extinct. ...
Chapter 28 PPt
Chapter 28 PPt

... Over geologic history, many animals and plants have lived and become extinct. ...
Journey to the Center of Earth
Journey to the Center of Earth

... Evidence for Continental Drift Fossils - Wegener learned that the fossils of an ancient reptile, Mesosaurus had been discovered in South America and western Africa. This small reptile lived about 270 million years ago. Its fossils were not found anywhere else in the world. Wegener said this fact co ...
Plate Tectonics
Plate Tectonics

... consists mostly of granite - a less dense igneous rock with larger crystals that is usually light in color. ...
Geologic Time and Earth`s Biological History
Geologic Time and Earth`s Biological History

... must be younger than the rock that it cuts.  Inclusion principle: Small fragments of one type of rock but embedded in a second type of rock must have formed first, and were included when the second rock was forming.  Charles Darwin (1809-1882) was an unpaid naturalist who signed up for a 5-yr expe ...
the_solid_earth
the_solid_earth

... The earth formed approximately 4.6 billion years ago from a nebular cloud of dust and gas that surrounded the sun. As the gas cooled, more solids formed. The dusty material accreted to the nebular midplane where it formed progressively larger clumps. Eventually, bodies of several kilometers in diame ...
Just how integrated is the Earth System
Just how integrated is the Earth System

... mechanical breakdown of rock (weathering), to form loose rock fragments and soil, and sculpts the surface of the Earth. ...
File
File

... lava cools instantly through contact with air and water.  The minerals do not have time to form, so they are microscopic.  Examples : obsidian, basalt ...
The Layer`s Of The Earth! - Doral Academy Preparatory
The Layer`s Of The Earth! - Doral Academy Preparatory

... • Oceanic crust: depth of 0-10 kilometres The majority of the Earth's crust was made through volcanic activity. The oceanic ridge system, a 40,000 kilometre network of volcanoes, generates new oceanic crust at the rate of 17 km3 per year, covering the ocean floor with an igneous rock called basalt. ...
Earth-Interior Foldable Notes
Earth-Interior Foldable Notes

... The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball sm ...
Exam I Review Q`s
Exam I Review Q`s

... What is luster? What is cleavage? How is hardness of minerals measured? What is the most abundant atom in the rocky part of the earth? What is the most abundant mineral in the crust? What are the minerals in the mantle? What is the liquidus? What is the solidus? What are the states of rocks found at ...
Slide 1
Slide 1

... earth’s surface -broken into more than a dozen slabs of rock called plates that rest on layer of the upper mantle -these plates carry earth’s oceans & continents ...
Earth-Interior Foldable Notes
Earth-Interior Foldable Notes

... The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball sm ...
Geothermal Energy - Faculty | Essex
Geothermal Energy - Faculty | Essex

... • Geothermal Energy has been around for as long as the Earth has existed. "Geo" means earth, and "thermal" means heat. So, geothermal means earth-heat. • Have you ever cut a boiled egg in half? The egg is similar to how the earth looks like inside. The yellow yolk of the egg is like the core of the ...
ppt wegener
ppt wegener

... The refraction and reflection of seismic waves as they move through one type of material to another is used to differentiate the layers of Earth’s interior. Earth has an inner and ...
Layers of the Earth
Layers of the Earth

... The asthenosphere is the layer of Earth that lies at a depth 100–250 km beneath Earth's surface. The asthenosphere gets its name from the Greek word for weak, asthenis, because of the relatively fragile nature of the materials of which it is made. It lies in the upper portion of Earth's structure tr ...
Inside the Earth
Inside the Earth

... The Core is Divided Into… Outer Core • The outer core is a liquid • The material of the outer core is considered molten as it is extremely hot • Less dense than the inner core • Made up of Iron and Nickel ...
Document
Document

... Review and Pre-Assess Objective: I will prepare to reach mastery on the unit test and assess what I know about the new unit. HW: complete review practice, prepare for test, project due Warm Up: Am I ready for the test? How much do I remember? * Answer the questions on the sheet ...
Chapter 5 Fast Changes on Earth
Chapter 5 Fast Changes on Earth

... 2. Movements in Earth’s crust caused by a sudden shift in Earth’s plates are __B__. 3. __C__ are areas where rocks slide past one another along cracks in the Earth’s plates. 4. When land becomes so full of water that it may change into a river of mud and rock, it is called a __G__. 5. An ocean wave ...
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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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