[Illustration: THE FOUR GREAT GLACIATIONS
_Six varying estimates of their duration made by five authorities. Fisk’s are of the New World glaciers, which are generally equated with those of Europe._]
There is one serious objection to Zeuner’s theory. Two of the three movements of the earth on which it is based would have reduced the warmth of summer in the northern hemisphere, but they would at the same time have increased the temperature of the southern hemisphere, thus alternating glaciation in the two hemispheres. Unfortunately, it is fairly well established that glaciers north and south of the equator have waxed and waned at the same time over a considerable number of years.
It is not enough, of course, to find the cause of the individual glaciations. There must be a cause for the glacial period as a whole. The Great Ice Age was an almost unique event in the history of the earth. We have to go back 200,000,000 years, to the time of the reptiles that preceded the dinosaurs, before we come again on major glaciations.
Zeuner states frankly that the astronomic theory “does not provide the cause of the Ice Age” as a whole.[11] Some added factor must be found. One which he considers is a migration of the north pole from the direction of the Pacific to its present location; Zeuner and others think the movement occurred before the Great Ice Age.
Two geologists, Maurice Ewing and William L. Donn, have accounted for the beginning of the Ice Age by accepting the theory that the north and south poles had moved from the north Pacific and the south Atlantic to their present positions. They account rather ingeniously for the advance and the retreat of the four glaciations. With the north pole where it is now, the ice-free Arctic Ocean would supply moisture by evaporation. This moisture, owing to cold over the northern areas of Asia and North America, would fall as snow to nourish glaciers. But how to stop this process and reverse it? It happens that the sea floor forms a rather high sill between the Atlantic and the Arctic Oceans. When the sea level dropped, as its water piled up in the great glaciers, the sill came too close to the surface to allow much of the warmer water from the Atlantic to reach the Arctic Ocean and to keep it from freezing over. Once the ice pack formed, evaporation diminished abruptly. The glaciers lost their nourishment. The summer melt returned their waters to the ocean. Sea level rose. The currents from the Atlantic could flow over the sill again and melt the ice pack. Then conditions would be ripe for a second advance of snow and ice across the northern world. The shallow waters of Bering Strait probably had little effect upon the Arctic Ocean.