वेदों की प्राचीनता एवं काल-निर्णय / ओरायन (लोकमान्य बाल गंगाधर तिलक - खगोलीय वैदिक शोध)

378 THE ARCTIC HOME IN THE VEDAS. cold climate; but in the present instance the climate of the Airyana Vaêjo was mild and genial before the invasion of Angra Mainyu, and we must, therefore, suppose that the Iranian table-land was not elevated at first, until Angra Mainyu upheaved it and produced a cold climate. But the present altitude of the plateau is not so great as to produce a winter of ten months, and this requires us again to assume the submergence of this land after the invasion of Angra Mainyu. Unfortunately there is no geological evidence forth-coming to support the upheaval and submergence of this land in the order mentioned above. But even if such evidence were forthcoming, the explanation would still fail to account why the inhabitants of Yima's Vara in the Airyana Vaêjo regarded a year as a single day, a description, which is true only at the North Pole. All attempts to locate the primitive Airyana Vaêjo in a region other than the circumpolar country must, therefore, be abandoned. The names of mythical rivers and countries may have been transferred in later times to real terrestrial rivers and provinces; but if we were to settle the position of the primitive rivers or countries by a reference to these new names, we can as well locate the Airyana Vaêjo between the Himâlay and the Vindhya mountains in India, for in later Sanskrit literature the land lying between these two mountains is called the Âryâvarta or the abode of the Aryans. The mistake committed by Darmesteter and Spiegel is of the same kind. Instead of determining the position of the Airyana Vaêjo from the fact that a winter of ten months is said to have been introduced therein by Angra Mainyu, and that a year seemed only as a day to the inhabitants thereof, they have tried to guess it from the uncertain data furnished by the names of rivers in Iran, though they were aware of the fact that these names were origi- nally the names of mythical rivers and were attached to the real rivers in Iran only in later times, when a branch of the