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Geological and solar climates

Chapter 14: TRANSCRIBER’S NOTE
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About This Book

The thesis investigates causes of past glacial and broader geological climate changes by examining geological evidence, fossil and moraine records, and the limits of correlation between continents. It reviews and critiques astronomical explanations, emphasizes the role of atmospheric composition and solar factors over orbital distance in controlling heat trapping, and considers how interpretation of stratigraphy and fossil plants informs climate reconstruction. The work argues for reevaluating prevailing theories and offers a physical explanation integrating terrestrial geography, atmospheric processes, and solar influences.

TRANSCRIBER’S NOTE

Page 6: “unequal subaerial denudation” changed to “unequal sub-aerial denudation”

Page 16: “two spheroidal iostherms” changed to “two spheroidal isotherms”

Page 25: “whole system of preglacial” changed to “whole system of pre-glacial”

Page 30: “at variance with those ante-dating” changed to “at variance with those antedating”

Page 31: “less in the Antartic” changed to “less in the Antarctic”

Page 33: “lowered one hundreed” changed to “lowered one hundred”

Page 35: “way into a subtropical growth” changed to “way into a sub-tropical growth”

Page 35: “are really coroborative” changed to “are really corroborative”

Page 46: “maintaining the cloud envelop” changed to “maintaining the cloud envelope”

Page 48: “light received by the earth” changed to “light received by the earth.”

Footnote 4: “la Mer. Déluges Périodique” changed to “la Mer. Déluges Périodiques”