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Baldur's Gate 3 is a role-playing video game with single-player and cooperative multiplayer elements. Players can create one or more characters and form a party along with a number of pre-generated characters to explore the game's story.
Baldur's Gate III: The Black Hound was a cancelled role-playing video game developed by Black Isle Studios for the Microsoft Windows platform. Announced in 2002 under the codenames FR6 and Project Jefferson, it was planned to be the third main entry in the Baldur's Gate series, utilizing the Dungeons & Dragons 3rd Edition ruleset.
Inquisitor is a 2009 role-playing video game developed by Czech company Cinemax. The game was in development for almost 10 years before its release in 2009. [1] [2] Three more years were needed to translate the game into English, and it was released on GOG.com on September 5, 2012. On June 1, 2013, Inquisitor was greenlit on Steam. [3]
Brine pools are created through three primary methods: brine rejection below sea ice, dissolution of salts into bottom water through salt tectonics, and geothermal heating of brine at tectonic boundaries and hot spots. Brine rejection: When sea water freezes, salts do not fit into the crystalline structure of ice, so the salts are expelled. The ...
The deepest portions of the hypolimnion often have lower oxygen concentrations than the surface waters (i.e., epilimnion). [4] While oxygen can typically exchange between surface waters and the atmosphere (i.e., in the absence of ice cover), bottom waters are comparatively isolated from atmospheric replenishment of oxygen.
Pelagic habitats are found near the surface or in the open water column, away from the bottom of the ocean. Demersal habitats are near or on the bottom of the ocean. An organism living in a pelagic habitat is said to be a pelagic organism, as in pelagic fish .
Water carried into the mantle eventually returns to the surface in eruptions at mid-ocean ridges and hotspots. [8] This circulation of water into the mantle and back is known as the deep water cycle or the geologic water cycle. [9] [10] [11] [5] Estimates of the amount of water in the mantle range from 1 ⁄ 4 to 4 times the water in the ocean ...
The bottom water of the Arctic Ocean is more isolated, due to the topography of the Arctic Ocean floor and the surrounding Arctic shelves. Deep Western Boundary Currents carry the Antarctic Bottom Water northward in the South Atlantic Ocean. The Antarctic Bottom Water shifts east when it reaches the equator, thus turning it into an eastern ...