N. H. Winchell on the Glacial features of Green Bay. 15 
No. 1, from a spot on the land of Mr. Robert Van Lear, 
about five miles (a Little age of) North from Staunton, in 
38° 14’ N. lat. and 79° O1’ W. long. 
No. 2, from the land of Mr. M. Fackler, about one mile to 
the San of the locality of No. 1. 
No. 8, about half a mile still further Southeast, or rather 
a little North of a N.W. and SE. line passing through the 
last named locality. 
It will be interesting to watch for the possible detection of 
other masses in the same neighborhood. 
This makes the fourth recorded instance of meteorites found 
within the State of Virginia, the three preceding having been, 
eteoric stone, which fell in Chesterfield Co., June 4th, 
1828, phe Jour. I, xv, 195 and xvi, 191). 
2. Meteoric iron, found in Grayson Co., described ce rof. 
Rogers of thee University i in 1842, ” Ghia Jour., I xlili, 169). 
3. Meteoric iron, found in Roanoke Co., and described by 
Prof. Houeres in 1842, (this Jour., I, xlin, 169). 
University of Virginia, March 27, 1871. 
Art. Il].—The Glacial Features of Green Bay of Lake Michigan, 
with some observations on a probable former outlet of Lake 
rato ae N. H. Wiscee, of the Geological Corps of 
Michiga 
THE topographical features of the region of Green Bay, are 
strikingly dependent on the geological structure as acted on by 
glacial forces. The west coast is low, and in but few places 
can the underlying rock be seen above the drift deposits. The 
immediate shore varies oie little from the rola trend - _ 
takes a direction nearly N. and &., an interesting fact, the special 
significance of which will be noticed further on. 
east coast is in the same way dependent on the line of 
piovien of the Niagara limestone; but, very unlike the west 
is frequent es indented by oa as fe LA Sees their great 
tiful ship hart ese real 
