Figure 4. Bangor quadrangle with ice-flow indicators plotted (modified from Syverson and Thompson, 2008). Southerly ice flow during the late Wisconsinan Glaciation flow maximum (red arrows) became strongly convergent (yellow arrows) along the axis of the Penobscot River valley as deglaciation proceeded. Brown Woods and the Interstate 395 interchange are referenced specifically in the text and figures.

Higher resolution PDF image of Figure 4 (826 Kb).

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Last updated on January 13, 2009

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