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Climate
Climate

... learned to adapt to normal climate variations. They choose certain crops and plant at certain seasons, according to their knowledge of local weather patterns. In an El Niño year, the weather may be ...
Wegener—Continental Drift
Wegener—Continental Drift

... supercontinent Pangaea and have drifted apart over time. This idea is known as continental drift. Which of the following is the best fossil evidence for continental drift? A. Fossils of the same land dwelling animals were found on widely separated continents. B. Fossils of the same ocean dwelling or ...
Sea-Floor Spreading
Sea-Floor Spreading

... - At the mid-ocean ridge, molten material rises from the mantle and erupts. The molten material spreads out, pushing older rock to both sides of the ridge. - Youngest rocks in the ocean are at the mid-ocean ridge; and the oldest are at the trench in the subduction zone. - Sea-Floor Spreading is the ...
The sea floor spreads apart at divergent boundaries.
The sea floor spreads apart at divergent boundaries.

... Mid-ocean ridges are the longest chain of mountains on Earth. Most of these ridges contain a rift valley along their center, as shown in the diagram below. When molten material rises from the asthenosphere, cold ocean water cools the rock until it becomes solid. As the plates move apart, new cracks ...
Notes
Notes

... The oceanic crust moves about ________________ centimeters per year. The melting crust will become a _______________________________  Oceanic to Oceanic form a ______________________________ zone. When 2 oceanic crusts collide they form an ocean _____________________. Ocean trenches are extremely__ ...
Sea Floor Spreading (SFS)
Sea Floor Spreading (SFS)

... the mid-ocean ridge. 2. When the hot magma comes into contact with the cold ocean water it cools and hardens and forms new oceanic crust (igneous rock). 3. Over millions of years the oceanic crust moves away from the mid-ocean ridge and towards the plate boundary with the continental crust. 4. When ...
CH 9 Plate tectonics
CH 9 Plate tectonics

... • Pie crust meets hand tossed) • Thinner and more sweet • Holds up better to washings • Able to leap tall buildings in a single bound. • Makes Jessica Alba look like a ho. ...
Six Weeks Test Review Key
Six Weeks Test Review Key

... 18. Describe a delta, including how it forms.________Deltas are triangular deposits of sediment found at the mouth of a river. They are formed due to deposition.________________ 19. How does a valley get its shape? ____valleys are carved by weathering and erosion due to the flow of a river or the mo ...
Sea Floor Spreading
Sea Floor Spreading

... Wegener could not explain how the continents moved but . . . • Harry Hess could! • He called his idea Sea Floor Spreading ...
scientific method
scientific method

... Beneath a very thin atmosphere, most of Earth’s surface is covered by a liquidwater ocean averaging 3,796 meters (12,451 feet) deep. ...
Plate Tectonics Lecture Notes Page
Plate Tectonics Lecture Notes Page

... Mantle: dense, hot layer of semi-solid rock Core ~ twice as dense as mantle b/c its metallic, not stony Earth's crust is literally only skin deep Oceanic Crust (basalt) ~10 km (6 mi) thick Continental Crust (granite) ~55 km (34 mi) thick Like an egg shell, Earth's crust is brittle & can break Lithos ...
Ocean Fertilization
Ocean Fertilization

... the release of nutrients, such as iron, into certain parts of the surface ocean. The oceans are currently responsible for removing a significant quantity of the CO2 added to the atmosphere by human activity each year, and this carbon may be sequestered in the ocean for hundreds of years. Iron can be ...
Plate Tectonics Unit(poster)
Plate Tectonics Unit(poster)

... *1 Youngest Rock was Found at the ridge and oldest the farthest away from the ridge *2 Basalt rock was found at the mid-ocean ridge, it comes from Volcanoes and makes the ocean floor of every ocean * 3 Ocean floor was found to be sinking below continents or other crust at the trenches… this process ...
ondernotes NATURal Science II Geology 1st Sem, 1st Exam
ondernotes NATURal Science II Geology 1st Sem, 1st Exam

...  “science of the earth” o Materials (minerals, rocks, etc.) o Processes (weathering, sedimentation, etc.) o Products (soil, etc.)  History of the planet’s life forms since its origin  The study of the Earth and other such solid bodies in space (moons, Mars, etc.)  It’s beginning is lost in antiq ...
Tectonic Plates &amp
Tectonic Plates &

... Seawater is a salt solution of nearly uniform composition. A solution is a homogenous mixture of two or more substances. Salinity is a measure of the amount of salt dissolved in seawater. On average, seawater is 96.5% water and 3.5% dissolved salts. If all the ocean water evaporated and the precipit ...
Label and Describe the Earth Diagram
Label and Describe the Earth Diagram

... Read the definitions then use the information to color code, label and describe IN YOUR OWN WORDS each section of the diagram below. Definitions: crust – (green) the rigid, rocky outer surface of the Earth, composed mostly of basalt and granite. The crust is the thinnest of all layers. It is thicker ...
Word Doc
Word Doc

... Maps (use latitude as the x-axis and longitude as the y-axis) Timeseries (use time as the x-axis and any other variable as the y-axis) Profiles (use depth as the y-axis and time or longitude as the x-axis) Variable vs. Variable diagrams (use any two variables for x and y axis) ...
Methodology Study area Results Introduction Conclusion Abstract
Methodology Study area Results Introduction Conclusion Abstract

... control them. The enhanced biogenic flux at SBBT during summer monsoon could be explained with the help of bottom-up control wherein the physical processes controlled chlorophyll biomass through nutrient supply. The mismatch between the lack of seasonality of biogenic flux at EIOT and seasonality in ...
Lecture 12: The Antarctic Circumpolar Current
Lecture 12: The Antarctic Circumpolar Current

... •South of the Polar Front, in the southwest Pacific, Sallee et al (2009) estimate an eddy-induced volume transport of 1.5 Sverdrups along the AAIW isopycnal layer. •In this small sector of the Southern Ocean, this eddy-induced transport would flux anthropogenic carbon into the interior at a rate ~0. ...
Arctic Ocean Paleoceanography and Future IODP Drilling
Arctic Ocean Paleoceanography and Future IODP Drilling

... Although the Arctic Ocean is a major player in the global climate/earth system, this region is one of the last major physiographic provinces on Earth where the short- and long-term geological history is still poorly known. This lack in knowledge is mainly due to the major technological/logistical pr ...
Earth Science
Earth Science

... Evidence of Continental Drift Evidence from Land Features 1. Continents fit together like the pieces to a puzzle  2. Mountain ranges on Africa and South America line up  3. European coal fields line up with North American coal fields. ...
Resource Booklet for IB practice question 11
Resource Booklet for IB practice question 11

... camouflage or to confuse predators • nets of tentacles to trap falling detritus for food • angler fish use light-producing bacteria that live on a special fishing rod-like fin that hangs over the angler’s head and wiggles in the water to attract prey • red or purple colouration (in normal light) e.g ...
Continental Drift - The Cyberworld of Deepsea Dawn, Oregon
Continental Drift - The Cyberworld of Deepsea Dawn, Oregon

... – PLATE TECTONICS – surface of earth composed of “plates” (LITHOSPHERE) that move on a “conveyor belt” (ASTHENOSPHERE) ...
Coral Current Connections I
Coral Current Connections I

... creates in the western Pacific drives evaporation of water vapor from the ocean into the atmosphere. That produces the highest rainfall of any region on Earth. The rising water vapor also sucks in more air from the east to replace it, strengthening the easterly trade winds. At times, however, the Pa ...
Earth Science Unit Review
Earth Science Unit Review

... boundaries, where material from the subducting plate rises to the surface. Shield volcanoes form over hot spots, which are weak parts of lithospheric plates where magma breaks through. 44. Students’ answers will vary but should include examples such as changes in water supply, change in biomes, incr ...
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Ocean



An ocean (from Ancient Greek Ὠκεανός, transc. Okeanós, the sea of classical antiquity) is a body of saline water that composes much of a planet's hydrosphere. On Earth, an ocean is one of the major conventional divisions of the World Ocean, which covers almost 71% of its surface. These are, in descending order by area, the Pacific, Atlantic, Indian, Southern, and Arctic Oceans. The word sea is often used interchangeably with ""ocean"" in American English but, strictly speaking, a sea is a body of saline water (generally a division of the world ocean) partly or fully enclosed by land.Saline water covers approximately 72% of the planet's surface (~3.6×108 km2) and is customarily divided into several principal oceans and smaller seas, with the ocean covering approximately 71% of Earth's surface. The ocean contains 97% of Earth's water, and oceanographers have stated that only 5% of the World Ocean has been explored. The total volume is approximately 1.35 billion cubic kilometers (320 million cu mi) with an average depth of nearly 3,700 meters (12,100 ft).As it is the principal component of Earth's hydrosphere, the world ocean is integral to all known life, forms part of the carbon cycle, and influences climate and weather patterns. It is the habitat of 230,000 known species, although much of the oceans depths remain unexplored, and over two million marine species are estimated to exist. The origin of Earth's oceans remains unknown; oceans are thought to have formed in the Hadean period and may have been the impetus for the emergence of life.Extraterrestrial oceans may be composed of water or other elements and compounds. The only confirmed large stable bodies of extraterrestrial surface liquids are the lakes of Titan, although there is evidence for the existence of oceans elsewhere in the Solar System. Early in their geologic histories, Mars and Venus are theorized to have had large water oceans. The Mars ocean hypothesis suggests that nearly a third of the surface of Mars was once covered by water, and a runaway greenhouse effect may have boiled away the global ocean of Venus. Compounds such as salts and ammonia dissolved in water lower its freezing point, so that water might exist in large quantities in extraterrestrial environments as brine or convecting ice. Unconfirmed oceans are speculated beneath the surface of many dwarf planets and natural satellites; notably, the ocean of Europa is estimated to have over twice the water volume of Earth. The Solar System's giant planets are also thought to have liquid atmospheric layers of yet to be confirmed compositions. Oceans may also exist on exoplanets and exomoons, including surface oceans of liquid water within a circumstellar habitable zone. Ocean planets are a hypothetical type of planet with a surface completely covered with liquid.
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