Hohokam Culture
The Hohokam is known primarily from the "core area" of the Phoenix
and Tucson basins, where perennial water sources were available. Known
as the Masters of the Desert, the Hohokam developed massive irrigation
systems consisting of hundreds of miles of canals. Some large villages
contained ballcourts and platform mounds. The Casa Grande Ruins
National Monument provides an example of the entire Hohokam temporal
sequence.
The Goldwater Range is located in the Papagueria, an area that
extends from the Avra Valley west of Tucson to the Colorado River,
from northern Mexico to an area just south of Gila Bend. Archeologists
consider this area to have been peripheral to the Hohokam core, and
was traversed by the Hohokam on shell gathering expeditions to the Sea
of Cortez.
As Hohokam population expanded to the west, large villages appeared
in eastern and northern Papagueria where shells were manufactured into
ornaments for trade with others. Some villages in the northern Santa
Rosa Valley included water reservoirs. Different regions produced
distinct patterns of pottery, such as Sells Red (from eastern
Papagueria), Phoenix basin red-on-buff and Tucson basin red-on-brown
ceramics.
Archaeological survey data from Organ Pipe Cactus National Monument
indicate major changes in Hohokam settlement during the Classic period
(A.D. 1150-1450). The majority of the 80 Hohokam sites recorded date
to the Classic period, indicating continued expansion or growth of
populations in western Papagueria. Hohokam sites are found for the
first time on the bajada. These artifact scatters with roasting pits
reflect resource procurement, processing, and preparation of plants
and animals found on the bajada. Previously-established villages
expanded with the addition of reservoirs. New villages, at least one
with a canal, were established. Tanque Verde Red-on-brown became the
dominant ceramic type along with Sells Red throughout the Classic
period. A new currently unnamed Redware that may have been
manufactured in the Organ Pipe area appeared for the first time. Late
Classic period sites include the addition of Salado polychromes. The
occurrence of Tucson basin ceramics indicates a shift either in
political alliances or exchange networks from the Phoenix basin to the
Tucson basin.
Large Classic period villages with reservoirs became increasingly
common
in this most arid portion of Papagueria. In an area where
permanent water supplies were almost nonexistent, reservoirs provided
a stable source of water which enabled year-round occupation. These
reservoirs did not merely collect water from the surrounding surface--
they were wells dug to intercept the shallow groundwater. Some
villages had canals which diverted and allocated water. Excavation and
maintenance of the reservoir required organized labor, which in turn
required a centralization of authority.
The Hohokam culture suffered a series of setbacks in the 1400s. A
massive flood of the Salt River destroyed large areas and canal
networks, and warfare between various groups resulted in destruction
of the great houses of the Salt and Gila River valleys. The Hohokam
people dispersed to various areas, and are claimed as the ancestors of
various other tribes, including the Hopi and O'odham. The large
villages were abandoned in favor of smaller, isolated settlements, and
the remaining Hohokam were assimilated into other groups. When Spanish
explorers arrived 200 years later, they encountered several O'odham
and other groups. When asked by the Spaniards who built the abandoned
great houses and villages, the answer was "Hohokam," meaning those who
lived here before and are "all used up."
http://www.luke.af.mil/rmo/pre.htm |