. Bulletin of the Geological Society of America. Geology. 520 J. H. STOLLER HISTORY OF MOHAWK-HUDSON REGION area of sand at the same elevation west of Saratoga Lake and separated from the Saratoga plain by a broad water-swept depression. In its origi- nal eastward extension the delta probably covered the area which now in- â A f 7V»*.,.).i-li'/ 3alls"fco« 5b«v?. Figure 1.âSketch Map of the lower Mohaivk-middle Hudson Region Showing the present drainage features and indicating the several courses of the Iro- quois-Mohawk River in late Pleistocene times and the deltas formed. T
. Bulletin of the Geological Society of America. Geology. 520 J. H. STOLLER HISTORY OF MOHAWK-HUDSON REGION area of sand at the same elevation west of Saratoga Lake and separated from the Saratoga plain by a broad water-swept depression. In its origi- nal eastward extension the delta probably covered the area which now in- â A f 7V»*.,.).i-li'/ 3alls"fco« 5b«v?. Figure 1.âSketch Map of the lower Mohaivk-middle Hudson Region Showing the present drainage features and indicating the several courses of the Iro- quois-Mohawk River in late Pleistocene times and the deltas formed. The deltas at Sche- nectady, north of Ballston Spa and at the mouth of Hoosic River were formed when Lake Albany was at its greatest development. The other deltas were formed at successive stages in the subsidence of the lake waters, as explained in the Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Geological Society of America. [New York : The Society]
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Keywords: ., bookcentury1800, bookdecade1890, booksubjectgeology, bookyear1890
