IN DESCENDING ORDER

_Southwestern and midwestern_

(11)

Togiak 80.1

(13)

Hooper Bay 79.7

(10)

Mumtrak 79.6

(6)

Pilot Station, Lower Yukon 79.3

(5)

Chukchee (Siberia) 78.6

(26)

Nelson Island 78

(6)

Southwestern Alaska 77.7

(32)

Indian Point (Siberia) 77.4

(12)

Little Diomede Island 77.4

(299)

St. Lawrence Island 77.2

(5)

Port Clarence 76.6

(34)

Pastolik and Yukon Delta 76.1

(14)

St. Michael Island 75.7

(116)

Nunivak Island 75.6

_Northwestern_

(222)

Point Hope 76.0

Kotzebue Sound and Kobuk (3)

River 75.4

(22)

Shishmaref 74.5

(101)

Point Barrow 74.1

(73)

Barrow 73.5

(33)

Wales 73.5

(7)

Golovnin Bay [152]72.6

(52)

Igloos, southwest of Barrow 69.7

_Northern and northeastern_

(7)

Hudson Bay and vicinity 76.3

(9)

Smith Sound 76.2

(15)

Southampton Island 74.8

(15)

Northern Arctic 73.6

(33)

Baffin Land and vicinity 73.2

(101)

Greenland 71.9

The Seward Peninsula shows sudden differences. There are a few

localities along its southern coast where the cranial type belongs

apparently to the Bering Sea and southern area. One site at Port

Clarence was one of these. But already at Golovnin Bay, which is

not far from Norton Sound and St. Michael Island, and according to

the evidence of the most recent collections (Collins 1928), also at

Sledge Island, there is a sudden appearance of marked dolichocrany,

which is repeated at Wales, on the western extremity of the peninsula,

approached at Shishmaref, the main Eskimo settlement on its northern

shore, and, judging from some fragmentary material seen at the

eastern end of the Salt Lake, also in the interior. The cause of this

distinctive feature in the Seward Peninsula is for the present elusive.

The little known territory urgently needs a thorough exploration.

The distribution of the cranial index farther north along the western

coast shows several points of interest. The first is the exceptional

position of Point Hope, one of the oldest and most populous settlements

in these regions, which by its cranial index seems to connect with the

Bering Sea groups. The second is the closeness, once more, of Barrow

and Point Barrow. The third and greatest is the presence, in a small

cluster of old igloos 8 miles down the coast from Barrow, of a group of

people that finds no counterpart in its cranial index and, as will be

seen later, also in some other characteristics, in the entire western

region; in fact, in the whole Eskimo territory outside of Greenland.

As noted before, the size of the head in this group is also closest to

that of Greenland. These peculiar facts indicate a problem that will

call for separate consideration.

The northern and northeastern groups, with the exception of the

mesocranic Hudson Bay and Smith Sound contingents, and the very

dolichocranic Greenlanders, show dolichocrany much the same as that of

Barrow and Point Barrow.

Anthropological Survey in Alaska · 第 345 / 471 题