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Building Earth`s Surface - Academic Resources at Missouri Western
Building Earth`s Surface - Academic Resources at Missouri Western

...  A point of the surface of the Earth directly above the focus  Seismograph  The instrument used to detect and measure the intensity of an earthquake  P, S, & L waves  Leave the focus at about the same time  Mercalli & Richter Scales  Tsunamai  Seismic sea wave ...
How do you think it formed?
How do you think it formed?

... -Made up of rock that is solid. -Farther down is hot enough to flow like putty. ...
2 Precambrian Geology
2 Precambrian Geology

... Early Hadean Highlights 1 • Earth formed about 4.6 billion years ago from coalescing interstellar dust. • Earth was bombarded by large planetesimals adding to earth’s mass (adds heat) • Hot spinning pre-earth mass melted, caused differentiation of materials according to density. • Distinct earth la ...
study guide - Hull Lessons
study guide - Hull Lessons

... During the 1500’s, geographers who made the first accurate maps noticed that the continents seemed to fit together like pieces of a jigsaw puzzle. The theory that says the earth’s surface is made up of about 20 moving pieces is called plate tectonics. Plate tectonics is the scientific theory that ex ...
Changing Earth Ch. 1 Review
Changing Earth Ch. 1 Review

... existed.  Pangaea ...
Earth Science and Climate Change - Brad Hubbard
Earth Science and Climate Change - Brad Hubbard

... sun when the rotating disc of dense, hot gasses coalesced into liquid droplets, and solidified as they continued to cool. Oldest rocks ~ 4.4 billion years old •  Inner planets (Mercury through Mars), closer to the sun, formed mostly from elements with relatively high melting points (Iron, Nickel, Al ...
practice exam. - UTEP Geology Homepage
practice exam. - UTEP Geology Homepage

... d. a major volcanic eruption of gas and dust, which contaminated the atmosphere and ...
Hadean and Archean
Hadean and Archean

... • Earth’s early atmosphere and hydrosphere were quite different than they are now • They also played an important role in the development of the biosphere • Today’s atmosphere is mostly – nitrogen (N2) – abundant free oxygen (O2) ...
History of Climate Change
History of Climate Change

... History of Climate Change  During earth’s history, climate has generally been warmer than it is today, but is periodically interrupted by short cooler periods.  Our climate today exists in one of those cooler periods. (last 2 million years) ...
Earth`s Interior Worksheet A Journey to the Center of the Earth (p. 9
Earth`s Interior Worksheet A Journey to the Center of the Earth (p. 9

... land? Mantle (p. 10 - 11) 8. What does the layer of mantle consist of? 9. What makes up the lithosphere? 10. Right below the lithosphere is a layer of mantle that is made of softer rock called the _________________________. 11. How deep is the mantle? Core (p. 11) 12. The earth’s core is made of two ...
Global Systems - Vocabulary Worksheet File
Global Systems - Vocabulary Worksheet File

... oceans, seas, lakes and rivers. 97.5% is saline and 2.5% is fresh, of which 68.7% is ice. The hydrosphere is mostly small molecules with dissolved ions. The cryosphere is that part of the hydrosphere where water is frozen. 4. Biosphere: The biosphere is the very thin layer in which all living organi ...
ESU-LT1-4
ESU-LT1-4

... Chapter 2 ...
Chapter 3 Test Review
Chapter 3 Test Review

... 15. During the process of nitrogen fixation, nitrogen gas is converted to_____________________ (88) 17. The acidity or basicity of a solution is described by the ____________________ scale. (71) 18. An ___________________ is the negatively charged part of an atom. (65) 19. As the asthenosphere moves ...
Plate Tectonics
Plate Tectonics

... 2. cycle of heating, rising, cooling, and sinking 3. theory that states that Earth's crust and upper mantle are broken into sections, which move around on a special layer of the mantle 4. area where an oceanic plate goes down ...
From the Beginning The earth and the whole universe were formed
From the Beginning The earth and the whole universe were formed

... along plate boundaries. It is also along these boundaries, that mountains form when _________________________ collide and the _________________________ tilts causing the land to be uplifted. Movement of shifting plates causes erupting molten lava to form _________________________. The Canadian Shiel ...
2.2 Notes
2.2 Notes

... - Both are made of iron and nickel. - The mantle is made of hot, dense rock. - It releases 80 percent of the heat generated from the earth’s interior. ...
Chapter 1.2-Spheres
Chapter 1.2-Spheres

... 2. Absorb, alter, block harmful solar radiation 3. Maintain constant temperature suitable for life ...
A historical overview of the work of Wegener
A historical overview of the work of Wegener

... Snider-Pelligrini (in 1858) was the first to suggest the continents had actually moved across Earth’s surface but he proposed the Great Flood as the cause. None could show evidence, apart from shape, that the continents had been joined.) Geologists at the time (c. 1912) dismiss Wegener as a ‘mere’ m ...
The Physical world
The Physical world

... another.—Think of an egg! • Core – solid metallic center made of nickel and iron • Mantle – soft layer of molten rock (magma) • Crust – thin layer of rock on earth’s surface ...
The Dynamic Earth: Plate Tectonics (PowerPoint)
The Dynamic Earth: Plate Tectonics (PowerPoint)

... http://smp.uq.edu.au/content/pitch-drop-experiment ...
Theme 8 – The Dynamic Earth: Plate Tectonics
Theme 8 – The Dynamic Earth: Plate Tectonics

... http://smp.uq.edu.au/content/pitch-drop-experiment ...
Forces Inside Earth
Forces Inside Earth

... Movement of continental plates creates great pressure inside the Earth ...
12earth6s
12earth6s

... Just the moon parts ...
Chapter 17 Vocabulary
Chapter 17 Vocabulary

... tectonic plates are moving apart; is associated with volcanism, earthquakes, and high heat flow, and is found primarily on the seafloor. Rift Valley (p. 456) Long, narrow depression that forms when continental crust begins to separate at a divergent boundary. Subduction (p. 457) Process by which one ...
03.02.03 Atmosphere, Hydrosphere, and
03.02.03 Atmosphere, Hydrosphere, and

... H. greenhouse effect __________________________________________________________________ ______________________________________________________________________________ ______________________________________________________________________________ ______________________________________________________ ...
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History of Earth



The history of Earth concerns the development of the planet Earth from its formation to the present day. Nearly all branches of natural science have contributed to the understanding of the main events of the Earth's past. The age of Earth is approximately one-third of the age of the universe. An immense amount of biological and geological change has occurred in that time span.Earth formed around 4.54 billion years ago by accretion from the solar nebula. Volcanic outgassing probably created the primordial atmosphere, but it contained almost no oxygen and would have been toxic to humans and most modern life. Much of the Earth was molten because of frequent collisions with other bodies which led to extreme volcanism. One very large collision is thought to have been responsible for tilting the Earth at an angle and forming the Moon. Over time, the planet cooled and formed a solid crust, allowing liquid water to exist on the surface.The first life forms appeared between 3.8 and 3.5 billion years ago. The earliest evidences for life on Earth are graphite found to be biogenic in 3.7-billion-year-old metasedimentary rocks discovered in Western Greenland and microbial mat fossils found in 3.48-billion-year-old sandstone discovered in Western Australia. Photosynthetic life appeared around 2 billion years ago, enriching the atmosphere with oxygen. Life remained mostly small and microscopic until about 580 million years ago, when complex multicellular life arose. During the Cambrian period it experienced a rapid diversification into most major phyla. More than 99 percent of all species, amounting to over five billion species, that ever lived on Earth are estimated to be extinct. Estimates on the number of Earth's current species range from 10 million to 14 million, of which about 1.2 million have been documented and over 86 percent have not yet been described.Geological change has been constantly occurring on Earth since the time of its formation and biological change since the first appearance of life. Species continuously evolve, taking on new forms, splitting into daughter species, or going extinct in response to an ever-changing planet. The process of plate tectonics has played a major role in the shaping of Earth's oceans and continents, as well as the life they harbor. The biosphere, in turn, has had a significant effect on the atmosphere and other abiotic conditions on the planet, such as the formation of the ozone layer, the proliferation of oxygen, and the creation of soil.
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