Climatic change and the gulf stream by

An almost easterly direction (azimuth of about 70° to 75^° of the Stream, as identified by the thermometer analysis, and Truxtun's eastern and southeastern flow reconfirm, to some extent, the correspondence found for the Iceland chronologies and Benjamin Franklin's maps.

Investigations of the Gulf Stream continued with a number of drift bottle experiments which charted tracks of over one hundred

Hans J. Stolle © 1975