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XXVI Congreso Internacional de Americanistas

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- 337 -<br />

During non-glacial times the mean monthly temperature at the pole<br />

WQuld run aboye 28° F. and perhaps up to 60° F . Or 70° F. in the<br />

summer. The polar region would have a cool, temperature humid climate.<br />

Frost would be unknown except perhaps aboye the Arctic Circie<br />

and on high mountains. In latitu<strong>de</strong>s between 65" N. and 8cf N., especially<br />

around the Arctic coast, there would be consi<strong>de</strong>rable areas with a<br />

climate similar .to the 11editerrmnca.n. The winters,however, would<br />

probably be cooler than the typical Mediterranean climate. Great stretches<br />

of ternpem.ture fJra..ss lands would obtain in northern Eurasia and<br />

North America. In the mountain areas along the western si<strong>de</strong>s of the<br />

continents aboye 50° N. latitu<strong>de</strong> where the southwesterly winds would<br />

have to rise to cross them, moisture would fall throughout the year.<br />

Bere, also, the cool-temperature-humid climate would prevai] with <strong>de</strong>ciduous<br />

forests and in the highest altitu<strong>de</strong>s, perhaps coniferous forests.<br />

Between latitu<strong>de</strong>s 35° N . and 50° N., the mountains along the west si<strong>de</strong><br />

oi the continents would probably have a M,editerrrmean type of climate.<br />

The proportion of arid lands would be increased. Great areas of <strong>de</strong>sert<br />

would prevail in the middle latitu<strong>de</strong>s, especially throughout the interiors<br />

of the continents. The regions is the ea'stern parts of the continents,<br />

having a monsoon climate would be greatly increased in size. Be:ow<br />

30Q N. latitu<strong>de</strong>, especially in North America a wet-and-dry-low-latitu<strong>de</strong><br />

climate would be the prevailing type.<br />

Throughout North America, north of the Tropic, two prehistoric<br />

culture horizons which have a vvorld-wi<strong>de</strong> distribution, are known.<br />

culture horizon is here <strong>de</strong>fined as a broad stage in culture growth which<br />

is i<strong>de</strong>ntified through the processes used in the satisfaction of the fundamental<br />

human needs. The earlier of the two horizons may be called<br />

the Osteic and is characterized by the following processes: absence<br />

of the agricultural process, absence of the true animal-domestication<br />

process, absence of the true house-building process, absence of the ceramic<br />

process, presence of the clothing process, weapons using on1y dire;:t<br />

muscular force in hurling the projectile, and implements ma<strong>de</strong> from bone,<br />

stone, shell, and wood, and certain special implements such as bla<strong>de</strong>s.<br />

gravo's, and 'weapon points. The later of the two horizons may be called<br />

the Ceramic. The following processes i<strong>de</strong>ntify it: the ful! agricultural<br />

process, domestication of animals, house-building process, the clothillg<br />

process, self-ejecting weapons, the ceramic process, implements other than<br />

ceramic ma<strong>de</strong> from bone, stone, shell, or wood, and certain special traits<br />

such as the grooved-ax, polished celt, pipe, mortar and grinding stones.<br />

The first great world horizon of which prehistory has concrete<br />

evi<strong>de</strong>nce is the Lithic. It covers in time the epoch from about the beginning<br />

of the Pleistocene to near the maximum of the W\irm-Wisconsin.<br />

T'wo culture areas of the Lithic beco me c1ifferentiated c1uring very early<br />

22<br />

A

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