lecture * 2011 japanese tsunami and wave properties
... but their frequency, f, remains the same because just as many waves pass any point. As a result their wavelength also gets smaller because =c/f. ...
... but their frequency, f, remains the same because just as many waves pass any point. As a result their wavelength also gets smaller because =c/f. ...
Open Ocean Notes
... Where is algae (phytoplankton) found in the open ocean? The surface zone Algae is the base of the open ocean food web Many open ocean animals stay in deep water during the day and surface at night to feed. ...
... Where is algae (phytoplankton) found in the open ocean? The surface zone Algae is the base of the open ocean food web Many open ocean animals stay in deep water during the day and surface at night to feed. ...
2013年1月12日托福写作真题回忆
... hope of explaining the enclosed seas, such as the Sea of Japan. These seas have a typical oceanic floor, except that the floor is overlaid by several kilometers of sediment. Their floors have probably been sinking for long periods. It seems possible that a sinking current of cooled mantle material o ...
... hope of explaining the enclosed seas, such as the Sea of Japan. These seas have a typical oceanic floor, except that the floor is overlaid by several kilometers of sediment. Their floors have probably been sinking for long periods. It seems possible that a sinking current of cooled mantle material o ...
Oceans - acpsd
... movement of ocean water (including waves, currents, and tides) on the ocean shore zone (including beaches, barrier islands, estuaries, and inlets). ...
... movement of ocean water (including waves, currents, and tides) on the ocean shore zone (including beaches, barrier islands, estuaries, and inlets). ...
Unit 3 Geology - Manatee School For the Arts / Homepage
... sea floor. The age of the rocks increases as one moves away from the rift zone. The midoceanic ridge is the primary site for sea-floor spreading. Earthquakes and volcanoes are where seafloor spreading is occurring. ...
... sea floor. The age of the rocks increases as one moves away from the rift zone. The midoceanic ridge is the primary site for sea-floor spreading. Earthquakes and volcanoes are where seafloor spreading is occurring. ...
The Structure and Origin of the Ocean Basins The water Planet
... The Mediterranean Sea is a semi-enclosed basin that extends for 3800 km in an East to West direction and for 800 km North to South in the widest sections. It covers an area of 2.5 million km2 and contains a volume of 3.7 million km3 of water. The average depth of the basin is thus 1500 m. Depths ove ...
... The Mediterranean Sea is a semi-enclosed basin that extends for 3800 km in an East to West direction and for 800 km North to South in the widest sections. It covers an area of 2.5 million km2 and contains a volume of 3.7 million km3 of water. The average depth of the basin is thus 1500 m. Depths ove ...
File
... ___________ (steep), and the __________________ _________ (at the base of the slope). o Sediments collect here. Abyssal Plains – are large, flat areas of the seafloor that extend across the deepest parts of the ocean basins. o _________ layers of sediment o Some underwater _________________ Mid-Ocea ...
... ___________ (steep), and the __________________ _________ (at the base of the slope). o Sediments collect here. Abyssal Plains – are large, flat areas of the seafloor that extend across the deepest parts of the ocean basins. o _________ layers of sediment o Some underwater _________________ Mid-Ocea ...
Список докладов, представленных на 50 EMBS и их абстракты
... particular year smoothers for each site, and site as fixed categorical factor. GAM2 included the same predictors except 6 particular smoothers. Likelihood ratio test did not reveal significant differences between models. Therefore we may consider the simpler GAM2 (R-sq = 0.26) as a better model indi ...
... particular year smoothers for each site, and site as fixed categorical factor. GAM2 included the same predictors except 6 particular smoothers. Likelihood ratio test did not reveal significant differences between models. Therefore we may consider the simpler GAM2 (R-sq = 0.26) as a better model indi ...
Tsunamis - GEOCITIES.ws
... the town of Aitape and wiped out entire communities along a 30km stretch of land. It was caused by two under sea earthquakes, measuring 7.0 on the Richter scale. By the time the waves hit the shore line they reached a height of 10meters. The communities had no warning and no where to go. Over 2,000 ...
... the town of Aitape and wiped out entire communities along a 30km stretch of land. It was caused by two under sea earthquakes, measuring 7.0 on the Richter scale. By the time the waves hit the shore line they reached a height of 10meters. The communities had no warning and no where to go. Over 2,000 ...
The Structure and Origin of the Ocean Basins The water Planet
... Often, where two continents lie close together, a smaller part of an ocean called a sea is formed. Mediterranean Sea, Red Sea, Arabian Gulf, the Gulf of Mexico, the Baltic Sea, North Sea, and South China Sea are examples of seas. Owing to their restricted connections with the open ocean, most margin ...
... Often, where two continents lie close together, a smaller part of an ocean called a sea is formed. Mediterranean Sea, Red Sea, Arabian Gulf, the Gulf of Mexico, the Baltic Sea, North Sea, and South China Sea are examples of seas. Owing to their restricted connections with the open ocean, most margin ...
Ocean Floor
... • Abyssal plain - the ocean floor (covers about 30% of the earth's surface). • The average water depth is around 5000 meters. Consists of a layer of unconsolidated sediment underlain by sedimentary rock and pillow basalt . ...
... • Abyssal plain - the ocean floor (covers about 30% of the earth's surface). • The average water depth is around 5000 meters. Consists of a layer of unconsolidated sediment underlain by sedimentary rock and pillow basalt . ...
Name: Date:______ Period:______ Lab – Sea Floor Spreading
... Introduction: Sea floor spreading is the hypothesis that the sea floor moves sideways away from the mid ocean ridge. The two sides of the ridge are moving in opposite directions leaving a rift valley that is the site of submarine volcanic eruptions. Molten rock from a magma chamber only 1 to 2 kilom ...
... Introduction: Sea floor spreading is the hypothesis that the sea floor moves sideways away from the mid ocean ridge. The two sides of the ridge are moving in opposite directions leaving a rift valley that is the site of submarine volcanic eruptions. Molten rock from a magma chamber only 1 to 2 kilom ...
Ocean Depth through Deep Time
... that the shape of seafloor age distribution is influenced by the growth of continental area over time, with an increasingly younger-aged, triangular shaped distribution favored for increasing continental surface. We also vary the amount of continents on Earth between 0, 10%, and 30% continents. Thes ...
... that the shape of seafloor age distribution is influenced by the growth of continental area over time, with an increasingly younger-aged, triangular shaped distribution favored for increasing continental surface. We also vary the amount of continents on Earth between 0, 10%, and 30% continents. Thes ...
jeopardyplatetech Answer Key
... What is the process by which new seafloor is continuously made at mid ocean ridges? When it comes to sea floor spreading, where would you find the youngest rocks? ...
... What is the process by which new seafloor is continuously made at mid ocean ridges? When it comes to sea floor spreading, where would you find the youngest rocks? ...
File - GAIA POWER PLANTS
... The Atlantis II Deep attains a maximum depth of 2,170 metres. Atlantis II Deep is noteworthy because it is one of the areas containing hot brines, with water temperatures ranging up to 56 °C and salinities to 270 parts per thousand, which is about 7 1/2 times that of normal seawater. Metallic trace ...
... The Atlantis II Deep attains a maximum depth of 2,170 metres. Atlantis II Deep is noteworthy because it is one of the areas containing hot brines, with water temperatures ranging up to 56 °C and salinities to 270 parts per thousand, which is about 7 1/2 times that of normal seawater. Metallic trace ...
Oceanography Quick Notes
... The ocean covers 70 % of the Earth. It contains dissolved salts with ions such as chloride, sodium, magnesium, and potassium. Salinity is a measure if the amount of salts dissolved in seawater. Almost all of the energy that heats up the oceans comes from the sun, but light and heat do not penetrate ...
... The ocean covers 70 % of the Earth. It contains dissolved salts with ions such as chloride, sodium, magnesium, and potassium. Salinity is a measure if the amount of salts dissolved in seawater. Almost all of the energy that heats up the oceans comes from the sun, but light and heat do not penetrate ...
Lecture 5: Oceans & Tides
... Photic Zone = illuminated zone of the ocean’s surface ~ Open Ocean: Water absorbs most light by 200 m ~ Coastal Zone: Due to suspended particles most light is absorbed in 10-50 m Apothic Zone = lightless zone beneath the surface ...
... Photic Zone = illuminated zone of the ocean’s surface ~ Open Ocean: Water absorbs most light by 200 m ~ Coastal Zone: Due to suspended particles most light is absorbed in 10-50 m Apothic Zone = lightless zone beneath the surface ...
Key - Scioly.org
... The continental margin is characterized by thick (and less dense) granitic rock of the continents. Near shore the features of the ocean floor are similar to those of the adjacent continents because they share the same granitic basement. Relatively thin (and denser) basalt forms the adjacent deep ...
... The continental margin is characterized by thick (and less dense) granitic rock of the continents. Near shore the features of the ocean floor are similar to those of the adjacent continents because they share the same granitic basement. Relatively thin (and denser) basalt forms the adjacent deep ...
Answer - Scioly.org
... 30. The layer of Earth that is rigid, mobile, and includes the continents is called the a. Asthenosphere b. Mesosphere c. Lithosphere d. Mantle 31. Name the three types of breaking waves. Mention the shape of the wave and ocean slope associated with each type. Spilling breakers = ocean floor has a g ...
... 30. The layer of Earth that is rigid, mobile, and includes the continents is called the a. Asthenosphere b. Mesosphere c. Lithosphere d. Mantle 31. Name the three types of breaking waves. Mention the shape of the wave and ocean slope associated with each type. Spilling breakers = ocean floor has a g ...
The Ocean Floor
... 4000 meters (3-25k ft)below the surface. Brrrr, you wouldn't want to visit the midnight zone. Temperatures are close to freezing The water is pitch-black Food is scarce ...
... 4000 meters (3-25k ft)below the surface. Brrrr, you wouldn't want to visit the midnight zone. Temperatures are close to freezing The water is pitch-black Food is scarce ...
Inner-Space Speciation Project
... Why Explore the Deep Sea? • The deep ocean is the largest living space on Earth • It’s properties are radically different from shallow ocean environments • Some of the oldest life forms live in the deep sea • Less than 1% of its volume has been explored • There is a high probability of discovering ...
... Why Explore the Deep Sea? • The deep ocean is the largest living space on Earth • It’s properties are radically different from shallow ocean environments • Some of the oldest life forms live in the deep sea • Less than 1% of its volume has been explored • There is a high probability of discovering ...
Topography of the Ocean Floor Notes
... Submarine Canyon – A deep, eroded area in the continental slope carved out by turbidity currents ...
... Submarine Canyon – A deep, eroded area in the continental slope carved out by turbidity currents ...
Sea
A sea is a large body of salt water that is surrounded in whole or in part by land. More broadly, the sea (with the definite article) is the interconnected system of Earth's salty, oceanic waters—considered as one global ocean or as several principal oceanic divisions. The sea moderates Earth's climate and has important roles in the water cycle, carbon cycle, and nitrogen cycle. Although the sea has been travelled and explored since prehistory, the modern scientific study of the sea—oceanography—dates broadly to the British Challenger expedition of the 1870s. The sea is conventionally divided into up to five large oceanic sections—including the IHO's four named oceans (the Atlantic, Pacific, Indian, and Arctic) and the Southern Ocean; smaller, second-order sections, such as the Mediterranean, are known as seas.Owing to the present state of continental drift, the Northern Hemisphere is now fairly equally divided between land and sea (a ratio of about 2:3) but the South is overwhelmingly oceanic (1:4.7). Salinity in the open ocean is generally in a narrow band around 3.5% by mass, although this can vary in more landlocked waters, near the mouths of large rivers, or at great depths. About 85% of the solids in the open sea are sodium chloride. Deep-sea currents are produced by differences in salinity and temperature. Surface currents are formed by the friction of waves produced by the wind and by tides, the changes in local sea level produced by the gravity of the Moon and Sun. The direction of all of these is governed by surface and submarine land masses and by the rotation of the Earth (the Coriolis effect).Former changes in the sea levels have left continental shelves, shallow areas in the sea close to land. These nutrient-rich waters teem with life, which provide humans with substantial supplies of food—mainly fish, but also shellfish, mammals, and seaweed—which are both harvested in the wild and farmed. The most diverse areas surround great tropical coral reefs. Whaling in the deep sea was once common but whales' dwindling numbers prompted international conservation efforts and finally a moratorium on most commercial hunting. Oceanography has established that not all life is restricted to the sunlit surface waters: even under enormous depths and pressures, nutrients streaming from hydrothermal vents support their own unique ecosystem. Life may have started there and aquatic microbial mats are generally credited with the oxygenation of Earth's atmosphere; both plants and animals first evolved in the sea.The sea is an essential aspect of human trade, travel, mineral extraction, and power generation. This has also made it essential to warfare and left major cities exposed to earthquakes and volcanoes from nearby faults; powerful tsunami waves; and hurricanes, typhoons, and cyclones produced in the tropics. This importance and duality has affected human culture, from early sea gods to the epic poetry of Homer to the changes induced by the Columbian Exchange, from Viking funerals to Basho's haikus to hyperrealist marine art, and inspiring music ranging from the shanties in The Complaynt of Scotland to Rimsky-Korsakov's ""The Sea and Sinbad's Ship"" to A-mei's ""Listen to the Sea"". It is the scene of leisure activities including swimming, diving, surfing, and sailing. However, population growth, industrialization, and intensive farming have all contributed to present-day marine pollution. Atmospheric carbon dioxide is being absorbed in increasing amounts, lowering its pH in a process known as ocean acidification. The shared nature of the sea has made overfishing an increasing problem.