The Seri Indians. (1898 N 17 / 1895-1896 (pages 1-344*))McGee, W J
History
The Seri Indians. (1898 N 17 / 1895-1896 (pages 1-344*))
McGee, W J
Seri Indians; Seri language; Yuman languages
In Seriland proper the distribution of potable water is conditioned by
the meager precipitation, the local configuration (shaped largely by
sheetflood erosion), and the disturbance of equilibrium of the scanty
ground-water due to the tilting of the province. The most abundant
permanent supply of fresh water is that of Arroyo Carrizal, which is
fed by drainage and seepage from the broad and lofty mass of pervious
rocks forming the southern part of Sierra Kunkaak, the abundant supply
being due to the fact that the eastern tributaries are energetically
retrogressing into the mass in deep gorges which effectually tap the
water stored during the semiannual storms. The arroyo and valley of
Agua Dulce are less favorably conditioned by reason of a trend against
the tilting of the province and by reason of the narrower and lower
mass of tributary rock in the northern part of the range, and the
flow is impermanent, as indicated by the absence of canes and other
stream plants; yet four explorers (Ugarte, 1721; Hardy, 1826; Espence,
1844; Dewey, 1875) reported fresh water, apparently in a shallow well
tapping the underflow, at the embouchure of the arroyo. On the eastern
slope of Sierra Kunkaak there are several arroyos which carry water
for weeks or even months after the winter rains, and sometimes after
those of summer; but the only permanent water—Tinaja Anita—is at the
base of a stupendous cliff of exceptionally pervious and easily eroded
rocks, so deeply cut that ground-water is effectually tapped, while
an adjacent chasm—Arroyo Millard—is so situated that the cliff-faced
spur of the sierra above the tinaja absorbs an exceptional proportion
of the surface flowage from the main crest. The tinaja (figure 3) is
permanent, as indicated by a canebrake some 20 by 50 feet in extent,
and by a native fig and a few other trees—though the dry-season
water-supply ranges from mere moisture of the rocks to a few gallons
caught in rock basins within the first 50 yards of the head of the
arroyo. No other permanent supplies of fresh water are known on the
island, though there are a few rather persistent tinajas along the
western base of Sierra Menor above Willard point.
Public-domain text, read in full here on John Shaqi.
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