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18 Feb

Thanks so much, Concerned Daughter Dear Concerned Daughter, When you say the tiny bug burrows under the skin, do you mean it just stays in that one spot under the skin, or does it travel, leaving a mark or track in it's wake? However, I don't believe there is any evidence that they burrow under the skin.

Does it cause the skin to itch or have any other reaction? They aren't known to burrow under the skin and stay there.

By late Antiquity mariners had very likely acquired intimate knowledge of coastal currents in the Mediterranean, but little about them was reported in the Classical works.

Following the dark and Middle Ages, when little progress was made, the voyages of discovery brought startling observations of many of Earth's most important ocean currents, such as the North and South Equatorial currents, the Gulf Stream, the Agulhas, Kuroshio, Peru, and Guinea currents, and others.

Perhaps because of the foregoing, many of the pioneering works, critical to establishing what the upper-level circulation is like, the majority of the charts accompanying them, and several of the groundbreaking theoretical treatments on the physics of currents, are only poorly known to present-day oceanographers.

In this paper we trace Western developments in knowledge and understanding of ocean circulation from the earliest times to the late-1800s transition into the modern era.

The tiny bug burrows under the skin and stays there. At first I thought she was scratching herself, but then she caught one to show me. Any help as to what they are or a remedy would be great.

They also believed in horrific whirlpools, a concept that persisted into the Renaissance and which would later provide subject material for modern literature.From the Greek Classical Age, we find hydrologic theories of Earth's interior being laced with subterranean channels (Socrates) and all motion deriving from a divine force forever propelling the heavens toward the west, the (Aristotle).These ideas, particularly the latter, dominated opinions about ocean circulation into the late Renaissance.During the next two decades, the western intensification of subtropical gyres was recognized (Wilkes) while numerous refinements were made to other global descriptions (Wilkes; Kerhallet; Findlay).Heuristic and often incorrect theories of what causes the circulations in the atmosphere and oceans were popularized in the 1850s and 1860s which led to a precipitous decline in the quality of charts intended for the public (Maury; Gareis and Becker).