The Brazil Current is a warm water current that flows south along the Brazilian south coast to the mouth of the Río de la Plata. This current is caused by diversion of a portion of the Atlantic South Equatorial Current from where that current meets the South American continent. It is a western boundary current like the Gulf Stream, and is indeed its southern counterpart; however, it is considerably shallower and weaker.It flows south from the equator to the west wind drift. It joins the Falkland Current at the Argentine Sea, making it a temperate sea.
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““I” is a militant social tendency, working to hold and enlarge its place in the general current of tendencies. So far as it can it waxes, as all life does. To think of it as apart from society is a palpable absurdity of which no one could be guilty who really saw it as a fact of life.”
—Charles Horton Cooley (1864–1929)