. Bulletin of the Geological Society of America. Geology. BELVIDERE AtfD LOWELL AREAS 42l According to the Hitchcock map, the serpentine bands, of which two are reported, terminate near the central part of Lowell township ; the west one, however, is represented as extending a little south of the village of Lowell. In Eden township no serpentine is represented. There / LEGEND AMPHI BOLITE. Figure I.—Geological Map of Belvidere Mountain. is, however, in Eden, and continuing in Lowell, a most interesting area of these magnesian rocks, forming the southern slope of Belvidere moun- tain, and a plat
. Bulletin of the Geological Society of America. Geology. BELVIDERE AtfD LOWELL AREAS 42l According to the Hitchcock map, the serpentine bands, of which two are reported, terminate near the central part of Lowell township ; the west one, however, is represented as extending a little south of the village of Lowell. In Eden township no serpentine is represented. There / LEGEND AMPHI BOLITE. Figure I.—Geological Map of Belvidere Mountain. is, however, in Eden, and continuing in Lowell, a most interesting area of these magnesian rocks, forming the southern slope of Belvidere moun- tain, and a plateau-like projection to the south and east of the mountain crest. This may be designated as the Belvidere area (see map, figure. 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
