Short-Hand Notes
... E) How the sun and moon create the tides 1) Tides – the rise and fall of water level on earth resulting from the gravitational pull of the moon and sun on the earth 2) The moon and suns gravity pull on all parts of the earth a) The moon pulls more than the sun because it is closer 3) Because land ca ...
... E) How the sun and moon create the tides 1) Tides – the rise and fall of water level on earth resulting from the gravitational pull of the moon and sun on the earth 2) The moon and suns gravity pull on all parts of the earth a) The moon pulls more than the sun because it is closer 3) Because land ca ...
New study to investigate the impacts of ocean acidification in the
... and brought into controlled conditions on deck. This natural seawater will be subjected to various levels of carbon dioxide that are likely to occur in the future. Dr Geraint Tarling, a British Antarctic Survey Researcher and the leader of this expedition says: “This is the most comprehensive invest ...
... and brought into controlled conditions on deck. This natural seawater will be subjected to various levels of carbon dioxide that are likely to occur in the future. Dr Geraint Tarling, a British Antarctic Survey Researcher and the leader of this expedition says: “This is the most comprehensive invest ...
What are the characteristics of a mineral?
... Tides- The rise and fall of the ocean water due to moon’s gravity and partly by the sun Continental shelf- Gentle sloping seabed near the land Continental slope- Outer edge of the continental shelf to the ocean floor Continental rise- Ocean floor between the continental slope and the abyssal plain. ...
... Tides- The rise and fall of the ocean water due to moon’s gravity and partly by the sun Continental shelf- Gentle sloping seabed near the land Continental slope- Outer edge of the continental shelf to the ocean floor Continental rise- Ocean floor between the continental slope and the abyssal plain. ...
Ocean habitats (“biozones”)
... If there is a difference, or gradient, between the inside and outside of the cell, an osmotic pressure will cause water molecules to move from high concentration of water (=low salinity) to low concentration of water (=high salinity). ...
... If there is a difference, or gradient, between the inside and outside of the cell, an osmotic pressure will cause water molecules to move from high concentration of water (=low salinity) to low concentration of water (=high salinity). ...
Surface Currents Activity
... Introduction: Surface waters of the Earth’s oceans are forced to move, primarily by winds. Where winds blow in the same direction for a long period of time, currents will develop that transport large masses of water over considerable distances across ocean surfaces. Objective: In this activity, you ...
... Introduction: Surface waters of the Earth’s oceans are forced to move, primarily by winds. Where winds blow in the same direction for a long period of time, currents will develop that transport large masses of water over considerable distances across ocean surfaces. Objective: In this activity, you ...
Factors that shape
... The origin of mountains (orogenesis) occurs after tectonic movements make rock layers fold and overlap. All the Earth’s surface, the lithosphere, is divided into rigid areas called continental plates and oceanic plates. These lithospheric plates continuously move and whenever they bump into each oth ...
... The origin of mountains (orogenesis) occurs after tectonic movements make rock layers fold and overlap. All the Earth’s surface, the lithosphere, is divided into rigid areas called continental plates and oceanic plates. These lithospheric plates continuously move and whenever they bump into each oth ...
Factors that shape
... The origin of mountains (orogenesis) occurs after tectonic movements make rock layers fold and overlap. All the Earth’s surface, the lithosphere, is divided into rigid areas called continental plates and oceanic plates. These lithospheric plates continuously move and whenever they bump into each oth ...
... The origin of mountains (orogenesis) occurs after tectonic movements make rock layers fold and overlap. All the Earth’s surface, the lithosphere, is divided into rigid areas called continental plates and oceanic plates. These lithospheric plates continuously move and whenever they bump into each oth ...
Ocean basin features
... It is clear that the Arctic Ocean is significantly shallower than the other oceans. Next, you will explore why. To do this, you will change the way the depth for each ocean is displayed. Currently, all depths are represented by a single shade of blue. You will load a new legend that classifies depth ...
... It is clear that the Arctic Ocean is significantly shallower than the other oceans. Next, you will explore why. To do this, you will change the way the depth for each ocean is displayed. Currently, all depths are represented by a single shade of blue. You will load a new legend that classifies depth ...
Planet Earth - Topic 4 (ANSWERS)
... Geological: in order for coal to be formed, it must have a tropical environment. Coal is found in many places where there is no tropical weather (Ex: Alberta). Most of the places were thought to be covered by glaciers. 5. What does SONAR stands for? When is it used? p. 386 Sound Navigation and Rangi ...
... Geological: in order for coal to be formed, it must have a tropical environment. Coal is found in many places where there is no tropical weather (Ex: Alberta). Most of the places were thought to be covered by glaciers. 5. What does SONAR stands for? When is it used? p. 386 Sound Navigation and Rangi ...
The Law of the Sea
... ocean-bottom plain that lies immediately offshore the continents. It averages between 200-500 feet in depth, and is separated from the “abyssal plain” (deep-ocean bottom averaging about 15,000 feet in depth) by a steep drop-off called the “continental slope.” C ti Continental t l shelf h lf is i the ...
... ocean-bottom plain that lies immediately offshore the continents. It averages between 200-500 feet in depth, and is separated from the “abyssal plain” (deep-ocean bottom averaging about 15,000 feet in depth) by a steep drop-off called the “continental slope.” C ti Continental t l shelf h lf is i the ...
Earth Science and Climate Change - Brad Hubbard
... • An incompressible fluid – nearly uniform density, depending slightly on salt content and temperature • Large heat capacity – 1000x that of the atmosphere – strong but slow effect on climate • Salty : typically 3.4% concentration by weight • Acidity: pH of 8.1, about 0.1 lower (25% higher acidi ...
... • An incompressible fluid – nearly uniform density, depending slightly on salt content and temperature • Large heat capacity – 1000x that of the atmosphere – strong but slow effect on climate • Salty : typically 3.4% concentration by weight • Acidity: pH of 8.1, about 0.1 lower (25% higher acidi ...
Ocean Features Objectives and HW
... Ocean trenches are formed when_. A. two oceanic plates slide past each other B. an oceanic plate goes under another oceanic plate C. two oceanic plates grind past each other along transform faults D. two oceanic plates hit each other causing both plates to rise up. ...
... Ocean trenches are formed when_. A. two oceanic plates slide past each other B. an oceanic plate goes under another oceanic plate C. two oceanic plates grind past each other along transform faults D. two oceanic plates hit each other causing both plates to rise up. ...
Virtual Integrated Science for Interactive Ocean Networked Systems (VISIONS05) Expedition
... Ridge in the northeast Pacific Ocean. At this site on the seafloor, where two of the planet’s great tectonic plates are spreading apart, animals live without sunlight at great depths and thrive on heat and chemicals venting from within the Earth. What is thought to be the first-ever transmission of ...
... Ridge in the northeast Pacific Ocean. At this site on the seafloor, where two of the planet’s great tectonic plates are spreading apart, animals live without sunlight at great depths and thrive on heat and chemicals venting from within the Earth. What is thought to be the first-ever transmission of ...
Where did the water for the oceans come from?
... •solar system evidence for heavy bombardment and models ...
... •solar system evidence for heavy bombardment and models ...
Layer Depth (km) Rigidity
... Origin of Atmosphere •Early H2 and He (light gases)-- “blown away” •Release of gases from interior N2, CO2, CH4, NH3, H2S, HCl, H2O vapor. •Evolution of atmosphere: (a) loss of reactive gases; (b) development of life – much later... CO2 removed and O2 accumulated. ...
... Origin of Atmosphere •Early H2 and He (light gases)-- “blown away” •Release of gases from interior N2, CO2, CH4, NH3, H2S, HCl, H2O vapor. •Evolution of atmosphere: (a) loss of reactive gases; (b) development of life – much later... CO2 removed and O2 accumulated. ...
Oceans: The Last Frontier
... An Emerging Picture of the Ocean Floor • Bathymetry – Mapping ocean depths and the shape, or topography, of the ocean floor – HMS Challenger – 1872-1876 • Traveled to every ocean except Arctic • Measured all types of properties, depths – Challenger Deep – deepest point –over 35,000ft ...
... An Emerging Picture of the Ocean Floor • Bathymetry – Mapping ocean depths and the shape, or topography, of the ocean floor – HMS Challenger – 1872-1876 • Traveled to every ocean except Arctic • Measured all types of properties, depths – Challenger Deep – deepest point –over 35,000ft ...
Currents
... • it flows from the Arctic Ocean south along the coast of Labrador and passes around Newfoundland, continuing south along the east coast of Nova Scotia • It meets the warm Gulf Stream at the Grand Banks southeast of Newfoundland and again north of the Outer Banks of North Carolina. The combination o ...
... • it flows from the Arctic Ocean south along the coast of Labrador and passes around Newfoundland, continuing south along the east coast of Nova Scotia • It meets the warm Gulf Stream at the Grand Banks southeast of Newfoundland and again north of the Outer Banks of North Carolina. The combination o ...
Water Unit Review - Paulding County Schools
... • Sarah’s family is trying to reduce the amount of water they use around their home. Using less water is one way to practice water ___. A.filtration. B.distribution. C.conservation. D.irrigation. ...
... • Sarah’s family is trying to reduce the amount of water they use around their home. Using less water is one way to practice water ___. A.filtration. B.distribution. C.conservation. D.irrigation. ...
Planet Earth - MSU Billings
... – Current atmosphere produced by biosphere (Oxygen) – Ocean composition influenced by biosphere precipitation of calcium carbonate – Fossils fuels – Fossils record past Earth environments • Current living species account for only 10% of known species throughout geologic history ...
... – Current atmosphere produced by biosphere (Oxygen) – Ocean composition influenced by biosphere precipitation of calcium carbonate – Fossils fuels – Fossils record past Earth environments • Current living species account for only 10% of known species throughout geologic history ...
Key concepts
... -know how to classify the layers of the earth by chemical composition AND by physical properties. Be able to name the layers using each classification scheme & describe their characteristics -know the difference between oceanic crust & continental crust -know how pressure and temperature change as y ...
... -know how to classify the layers of the earth by chemical composition AND by physical properties. Be able to name the layers using each classification scheme & describe their characteristics -know the difference between oceanic crust & continental crust -know how pressure and temperature change as y ...
Earth Science Chapter 20 20.1 The Water Planet 20.1 The Water
... oceans, and samples of ocean water, sediments, and 1000’s forms of marine life. Joides Resolution ...
... oceans, and samples of ocean water, sediments, and 1000’s forms of marine life. Joides Resolution ...
ROCKING AND ROLLING By Philip Steele DOWN UNDER Our
... Our planet Earth is huge — about 3,960 miles from the surface to the center. Walking this far would take you about 55 days and nights. You wouldn’t be able to walk to the center of the earth, though, as it’s incredibly hot. It’s at least 9,000oF, which is nearly the same temperature as the surface o ...
... Our planet Earth is huge — about 3,960 miles from the surface to the center. Walking this far would take you about 55 days and nights. You wouldn’t be able to walk to the center of the earth, though, as it’s incredibly hot. It’s at least 9,000oF, which is nearly the same temperature as the surface o ...
ES Chapter 9 Study Guide
... 2. What does evidence about ancient climates indicate? 3. What evidence does the distribution of the swimming reptile Mesosaurus provide? 4. What is the main reason Wegener’s continental drift hypotheses was rejected? 5. In the plate tectonic theory, the lithosphere is divided into how many major pl ...
... 2. What does evidence about ancient climates indicate? 3. What evidence does the distribution of the swimming reptile Mesosaurus provide? 4. What is the main reason Wegener’s continental drift hypotheses was rejected? 5. In the plate tectonic theory, the lithosphere is divided into how many major pl ...
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.