40 FTET.D MUSEUM OE NATURAL HISTORY 
Relief map of Europe. Horizontal scale, 85 miles to 1 inch. 
Vertical scale, 45 times the horizontal. 
Relief map of Asia. Horizontal scale, 216 miles to 1 inch. 
Vertical scale, 39 times the horizontal. 
Relief map of Africa. Horizontal scale, 184 miles to 1 inch. 
Vertical scale, 53 times the horizontal. 
Relief map of North America. Horizontal scale, 140 miles to 
1 inch. Vertical scale, 39 times the horizontal. 
Relief map of South America. Horizontal scale 147 miles to 
1 inch. Vertical scale 30 times the horizontal. 
Relief map of the United States. Horizontal scale, 85 miles 
to 1 inch. Vertical scale, 36 times the horizontal. 
Geological map of the State of New York. 
Relief map of the State of New York. Horizontal scale, 1 
inch equals 12 miles. Vertical scale, 5 to 1. The former bed of 
Lake Iroquois is shown, also the plateau-like character of the 
southern part of the state. 
Relief map of New York City and vicinity. Horizontal scale, 
1 inch equals 1 mile. Vertical scale, 3 to 1. The relations of 
land and water which have given New York its great commercial 
importance are well shown. 
Physical map of the British Isles. 
Relief map of Palestine. Horizontal scale, ^ of an inch 
equals 1 mile. Vertical scale, Syi times the horizontal. 
Geological map of the State of Illinois. 
Series of four maps showing the successive stages in the re- 
cession of Lake Chicago, following the Glacial period, and the 
development of the Chicago plain. Former beach lines, spits 
and islands are well marked by the topography. 
Relief map of northeastern Illinois, including Cook, Du 
Page, Will, and eighteen adjoining counties. The course of the 
Chicago Drainage Canal is shown. 
Relief map of the region of extinct volcanoes in Auvergne, 
central France; geological and topographical. 
Relief map of the State of Nebraska. Horizontal scale, 1 
inch equals 5 miles. Vertical scale, 1 inch equals 2,000 feet. 
On tables or in cases occupying the floor of the hall will be 
found the following : 
Harvard geographical models, showing respectively the effect 
of submergence and elevation of a coastal region. 
