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Page 5210, results 130226 - 130250

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Bedrock topography of north-central Iowa
R.E. Hansen
1978, IMAP 1080
The bedrock in Iowa (Hershey, 1969) is generally overlain by deposits of glacial drift and alluvium, which range in thickness from less than 1 ft to more than 400 ft, and from less than 1 ft to about 60 ft respectively. The configuration of the bedrock surface is the result...
Geologic map of the Casius Quadrangle of Mars
R. Greeley, J. E. Guest
1978, IMAP 1038
Geologic units of the martian surface are subdivided on the basis of surface morphology, albedo, and crater distribution and are placed in a stratigraphic sequence following principles of superposition, crosscutting relations, and, to a degree, crater density. The Casius quadrangle (30˚ N to 65˚ N lat; 240˚ W...
Geologic map of the Amazonis Quadrangle of Mars
E. C. Morris, S.E. Dwornik
1978, IMAP 1049
The Amazonis quadrangle lies within the northern sparsely cratered hemisphere of Mars (Carr and others, 1973) The dominant structural ad physiographic features of the quadrangle are...
Geologic map of the New Windsor Quadrangle, Carroll County, Maryland
G.W. Fisher
1978, IMAP 1037
The pattern of rock units in the geologic map of the New Windsor quadrangle has been affected by three distinguishable generations of folds; following the usage of Tobisch and Fleuty (1969) and Higgins (1973), the fold generations are named for localities where they are well displayed....
Geologic map of the Aeolis Quadrangle of Mars
D. H. Scott, M.N. West
1978, IMAP 1111
Two principal physiographic provinces of Mars are represented in the Aeolis quadrangle: (1) Elysium Planitia in the north is part of a broad planet-encircling belt of relatively young lowland plains, and (2) cratered highlands in the south consist<span...