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The
Pensauken was initially described by Rollin D. Salisbury as the "Second Stage of the Yellow Gravel", with the first stage being the Beacon Hill Formation, the third being the Jamesburg Formation, and the fourth being the
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The
Pensauken is described as "Fine-to-coarse sand, minor silt and very coarse sand; reddish-yellow to yellow; pebble gravel." It may be massive (without stratification) or
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Surficial geology of the Camden and
Philadelphia quadrangles, Camden, Gloucester, and Burlington counties, New Jersey
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Shattuck, G.B., 1901, The
Pleistocene problem of the north Atlantic Coastal Plain:
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194:. New Jersey Geological Survey. Open-file Map OFM 60. Map Scale: 1:24,000.
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The formation is named after exposures near the mouth of
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National
Geologic Map Database, Geolex – Unit Summary,
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Annual Report of the State
Geologist for the year 1893
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Northeastern United States geologic formation stubs
205:Johns Hopkins University Circular, v. 20, no. 152
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161:Surface Geology Report of Progress
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287:Geologic formations of New Jersey
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229:This article about a specific
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240:. You can help Knowledge by
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297:New Jersey geography stubs
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188:Scott D. Stanford, 2004.
80:Rollin D. Salisbury (1893)
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159:Rollin D. Salisbury,
236:in New Jersey is a
88:Pensauken Formation
22:Pensauken Formation
131:Cape May Formation
121:, and may contain
92:geologic formation
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108:Pennsylvania
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281:Categories
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119:stratified
110:, of Late
104:New Jersey
46:New Jersey
234:formation
178:Pensauken
31:Formation
112:Tertiary
100:Maryland
96:Delaware
77:Named by
58:Maryland
54:Delaware
37:Location
64:Country
106:, and
42:Region
114:age.
90:is a
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