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The Pleistocene of North America and its vertebrated animals from the states east of the Mississippi River and from the Canadian provinces east of longitude 95°

Hay, Oliver Perry · Public domain text

238,132 words · about 16 h 41 min to read

About this edition

The text of The Pleistocene of North America and its vertebrated animals from the states east of the Mississippi River and from the Canadian provinces east of longitude 95° comes from Project Gutenberg e-text #61765. It is public domain in the United States. Project Gutenberg’s header and license text are removed, and RedLectern sets the text out for reading on screen; no words of the book are rewritten or summarized. More formats (EPUB, Kindle) · How RedLectern is built

This text-only edition leaves out 68 illustrations. See the illustrated edition at Project Gutenberg.

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About this book

Author
Oliver Perry Hay (1846–1930)
Language
English
Subjects
Paleontology › Pleistocene, Paleontology › North America, Vertebrates, Fossil
Length
238,132 words · about 16 h 41 min
Sections
4 reader sections · Table of contents
Contents (4)

The opening of Preface

The writer has been engaged for several years on an investigation of the Pleistocene geology of North America and of the Vertebrata which have been discovered in the deposits of this epoch. It had been his expectation to publish the results of all his studies at the same date. However, on consultation with Dr. John C. Merriam, it was agreed that it would be better to publish immediately that part which pertains to the region lying east of the Mississippi River and, as to the country further north, that east of longitude 95°.

At the outset the writer was convinced that, before just conclusions could be reached, it was necessary to know what fossil materials had been collected and under what geological and geographical conditions. He therefore made as thorough a search as possible of the literature for reports of discoveries of fossil vertebrates. Also, when in scientific journals or in newspapers the finding of fossils was recorded, recourse was had to correspondence, thus securing much exact information as to locality, kind of matrix, depth, and other important data. Often photographs have been obtained and even the materials themselves.

Read on in Part 2 →