Ocean current the windthe Coriolis effect plays a role in their behaviours. The thermohaline circulation is a part of the large-scale ocean circulation that is driven by global density gradients created by surface heat and freshwater fluxes. The adjective "thermohaline" derives from "thermo-" referring to temperature and "" referring to salt content, factors which together determine the density of sea water. Wind-driven surface currents (such as the Gulf Stream) travel polewards from the equatorial Atlantic Ocean, cooling en route, and eventually sinking at high latitudes (forming North Atlantic Deep Water). This dense water then flows into the ocean basins. While the bulk
Western Europe Atlantic Current. Western European languages mostly fall within two Indo-European language families: the Romance languages, descended from the Latin of the Roman Empire; and the Germanic languages, whose ancestor language (Proto-Germanic) came from southern Scandinavia. Romance languages are spoken primarily in the southern and central part of Western Europe, Germanic languages in the northern part (the British Isles and the Low Countries), as well as a large part of Northern and Central Europe. Other Indo-European languages include the Celtic group (that is, Irish, Scottish Gaelic, Manx, Welsh, Cornish, and Breton). Basque is the only currently living Western European language isolate.