The "'sea of Chilo?"'( Spanish : " Mar de Chilo?" or " Mar Chilote " ) is a marginal sea of the coast of Chile that is separated from the Pacific Ocean by Chilo?Island.
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A "'marginal sea "'is a division of an ocean, partially enclosed by islands, archipelagos, or peninsulas, adjacent to or widely open to the open ocean at the surface, and / or bounded by submarine ridges on the sea floor.
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The big rivers Ob and Yenisei, among others, flow from the south into this marginal sea of the Arctic Ocean, their abundant waters contributing to a climate with relatively high precipitation despite the prevalent extreme cold temperatures of the high latitude.
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Point Barrow is also an important geographical landmark, marking the limit between two marginal seas of the Arctic, the Chukchi Sea on its western side and the Beaufort Sea on the eastern, both delimited to the North by the edge of the map as seen here.
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The "'Pacific Ocean "'as example of terminology concerning seas : the area inside the black line includes the seas included in the Pacific Ocean prior to 2002 and the darker blue areas are its informal current borders, following the recreation of the Southern Ocean and the reinclusion of marginal seas.
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""'Coregonus sardinella " "', known as the "'sardine cisco "', and in North America as the "'least cisco "', is a brackishwater species of salmonid fish that inhabits rivers, estuaries and coastal waters of the marginal seas of the Arctic Basin, as well as some large lakes of those areas.
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Recently, work has compiled and scaled available data on CO 2 fluxes in coastal environments, and shown that globally marginal seas act as a significant CO 2 sink (-1.6 mol C m " 2 y " 1;-0.45 Gt C y " 1 ) in agreement with previous estimates.
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In all, water from oceans and marginal seas, saline groundwater and water from saline closed lakes amount to over 97 % of the water on Earth, though no closed lake stores a globally significant amount of water . " Saline " groundwater is seldom considered except when evaluating water quality in arid regions.
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During the Triassic, the Franconian part of these depressions was often part of the mainland, in the Jurassic it was covered for most of the time by a marginal sea of the western erosion and weathering ( especially in the Jura in the form of karst ), which has ultimately led to formation of today's landscapes.
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The "'Sea of Okhotsk "'(; ) is a marginal sea of the western Pacific Ocean, lying between the Kamchatka Peninsula on the east, the Kuril Islands on the southeast, the island of Hokkaido to the south, the island of Sakhalin along the west, and a long stretch of eastern Siberian coast ( the Shantar Sea ) along the west and north.
