Climate and Time in Their Geological Relations: A Theory of Secular Changes of the Earth's Climate

amount of heat antarctic aphelion arctic regions Atlantic beds bottom boulder clay Caithness Carboniferous cause consequently considerable density denudation deposits depth descend difference of specific difference of temperature earth's orbit eccentricity ecliptic effect Eocene equal equator equatorial column equatorial regions evidence extent fact feet flow foot-pounds force Geol geological geologists glacial epoch glacier globe Grangemouth greater Greenland Gulf-stream heat received ice-cap icebergs inter-tropical John Herschel land land-ice latitude lower mass mean temperature melting miles Miocene molecules motion North North Sea northern obliquity ocean-currents oceanic circulation perihelion polar column polar regions poles present probably produce Professor quantity of heat radiation regard result river rocks sand Scotland sea-bottom sea-level shear slope snow and ice southern hemisphere specific gravity Straits of Florida stratified stream striated submergence summer sun's supposed surface theory thickness tion tropical warm periods warm water winds winter