Climate and Time in Their Geological Relations: A Theory of Secular Changes of the Earth's ClimateAppleton, 1890 - 577 páginas |
Dentro del libro
Resultados 1-5 de 35
Página ii
... APHELION . S. P. Glacial N.P. Difference between aphelion & perihelion distance 14 , 212,700 miles . N. WINTER SOLSTICE IN THEIR GEOLOGICAL RELATIONS : A THEORY OF SECULAR CHANGES. N.WINTER N. SUMMER pter Clacity 200 69 DAYS . Perihelion ...
... APHELION . S. P. Glacial N.P. Difference between aphelion & perihelion distance 14 , 212,700 miles . N. WINTER SOLSTICE IN THEIR GEOLOGICAL RELATIONS : A THEORY OF SECULAR CHANGES. N.WINTER N. SUMMER pter Clacity 200 69 DAYS . Perihelion ...
Página viii
... Aphelion than in Perihelion . - Pro- fessor Tyndall on the Glacial Epoch . - A general Reduction of Tem- perature will not produce a Glacial Epoch . - Objection from the present Condition of the Planet Mars PAGI · 54 CHAPTER V. REASON ...
... Aphelion than in Perihelion . - Pro- fessor Tyndall on the Glacial Epoch . - A general Reduction of Tem- perature will not produce a Glacial Epoch . - Objection from the present Condition of the Planet Mars PAGI · 54 CHAPTER V. REASON ...
Página 14
... aphelion , and to raise to nearly as great an extent the temperature of the opposite hemisphere , whose winters of course occur in perihelion . Until attention was directed to those physical circumstances to which I refer , it was ...
... aphelion , and to raise to nearly as great an extent the temperature of the opposite hemisphere , whose winters of course occur in perihelion . Until attention was directed to those physical circumstances to which I refer , it was ...
Página 17
... aphelion , has , for reasons which are explained in Chapter IV . , its temperature lowered , while that of the opposite hemisphere is raised . Let us suppose the northern hemisphere to be the cold one , and the southern the warm one ...
... aphelion , has , for reasons which are explained in Chapter IV . , its temperature lowered , while that of the opposite hemisphere is raised . Let us suppose the northern hemisphere to be the cold one , and the southern the warm one ...
Página 54
... Aphelion than in Perihelion . - Professor Tyndall on the Glacial Epoch . - A general Reduction of Temperature will not produce a Glacial Epoch . - Obj - ction from the present Condition of the Planet Mars . Primary cause of Change of ...
... Aphelion than in Perihelion . - Professor Tyndall on the Glacial Epoch . - A general Reduction of Temperature will not produce a Glacial Epoch . - Obj - ction from the present Condition of the Planet Mars . Primary cause of Change of ...
Otras ediciones - Ver todas
Términos y frases comunes
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