geomorphology

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Notes on the Mesozoic strata of Virginia
W. M. Fontaine

American Journal of Science March 1879, s3-17 (99) 229-239; DOI: https://doi.org/10.2475/ajs.s3-17.99.229
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Valley of the Minnesota River and of the Mississippi River to the junction of the Ohio; its origin considered
G. K. Warren

American Journal of Science December 1878, s3-16 (96) 417-431; DOI: https://doi.org/10.2475/ajs.s3-16.96.417
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Relative agency of glaciers and sub-glacial streams in the erosion of valleys
W. H. Niles

American Journal of Science November 1878, s3-16 (95) 366-370; DOI: https://doi.org/10.2475/ajs.s3-16.95.366
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On the artificial mounds of northeastern Iowa, and the evidence of the employment of a unit of measurement in their erection
W. J. McGee

American Journal of Science October 1878, s3-16 (94) 272-278; DOI: https://doi.org/10.2475/ajs.s3-16.94.272
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History of cavern exploration in Devonshire, England
W. Pengelly

American Journal of Science October 1877, s3-14 (82) 299-308; DOI: https://doi.org/10.2475/ajs.s3-14.82.299
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On Dr. Peale's Notes on the age of the Rocky Mountains in Colorado
John James Stevenson

American Journal of Science April 1877, s3-13 (76) 297-299; DOI: https://doi.org/10.2475/ajs.s3-13.76.297
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Notes on the age of the Rocky Mountains in Colorado
A. C. Peale

American Journal of Science March 1877, s3-13 (75) 172-181; DOI: https://doi.org/10.2475/ajs.s3-13.75.172
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The Colorado Plateau province as a field for geological study
G. K. Gilbert

American Journal of Science August 1876, s3-12 (68) 85-103; DOI: https://doi.org/10.2475/ajs.s3-12.68.85
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The Geological Survey of Brazil; first preliminary report made to the counsellor Thomaz Jose Coelho de Almeida, Minister and Secretary of State for Agriculture, etc
C. F. Hartt

American Journal of Science June 1876, s3-11 (66) 466-473; DOI: https://doi.org/10.2475/ajs.s3-11.66.466
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On southern New England during the melting of the great glacier; Part IV
James D. Dana

American Journal of Science December 1875, s3-10 (60) 409-438; DOI: https://doi.org/10.2475/ajs.s3-10.60.409

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