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Plants of Casa Grande Ruins National Monument - NPS Inventory ...

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and groundwater were used (Powell et al. 2006). By 1928, the construction <strong>of</strong><br />

Coolidge Dam ended the era <strong>of</strong> the Gila as a free-flowing river through the area.<br />

The conversion <strong>of</strong> the landscape to agriculture continued unabated, and had<br />

encircled the monument by 1932.<br />

Agriculture in the Coolidge area suffered greatly from overpumping <strong>of</strong> the water<br />

table, which was obvious as the water level <strong>of</strong> the park’s well dropped from<br />

128 feet below the surface, in the early 1940s, to more than 300 feet below the<br />

surface by 1956 (Clemensen 1992, Powell et al. 2006). This lowering <strong>of</strong> the water<br />

table, combined with a widespread mistletoe infestation, contributed to a large<br />

scale die-<strong>of</strong>f <strong>of</strong> the <strong>Casa</strong> <strong>Grande</strong> <strong>Ruins</strong> mesquite population in the 1930s (Judd<br />

et al. 1971). The decade <strong>of</strong> the 1930s also saw the bulk <strong>of</strong> the development at the<br />

monument, with construction <strong>of</strong> the ro<strong>of</strong> over the ruins in 1932 and, by the end<br />

<strong>of</strong> the decade, the visitor center, paths, roads, and several outbuildings. These<br />

are the same buildings that constitute the monument today. There has been only<br />

one major excavation <strong>of</strong> the ruin complexes; at that time, vegetation was scraped<br />

<strong>of</strong>f the site entirely. Since the 1930s, little has been done to alter or manipulate<br />

the vegetation at <strong>Casa</strong> <strong>Grande</strong> <strong>Ruins</strong>. Today, some studies have questioned<br />

the negative effects <strong>of</strong> pesticide drift from neighboring agricultural land; this,<br />

combined with the edge effects <strong>of</strong> rapidly urbanizing Pinal and Maricopa<br />

counties, the continued decline <strong>of</strong> the water table, and active climate change, all<br />

have serious ecological implications for <strong>Casa</strong> <strong>Grande</strong> <strong>Ruins</strong> NM.<br />

Clemensen, A.B. 1992. A centennial history <strong>of</strong> the first prehistoric reserve:<br />

1892-1992. United States Department <strong>of</strong> the Interior. <strong>National</strong> Park<br />

Service, Washington, D.C.<br />

Judd, B.I., J.M. Laughlin, H.R. Guenther, and R. Handegarde. 1971. The lethal<br />

decline <strong>of</strong> mesquite on the <strong>Casa</strong> <strong>Grande</strong> Ruin <strong>National</strong> <strong>Monument</strong>.<br />

Great Basin Naturalist 31: 152-159.<br />

Powell, B. F, E. W. Albrecht, C. A. Schmidt, W. L. Halvorson, P. Anning,<br />

and K. Docherty. 2006. Vascular Plant and Vertebrate <strong>Inventory</strong> <strong>of</strong><br />

<strong>Casa</strong> <strong>Grande</strong> <strong>Ruins</strong> Naitonal <strong>Monument</strong>. OFR 2005-1185. U.S.<br />

Geological Survey, Southwest Biological Science Center, Sonoran<br />

Desert Research Station, University <strong>of</strong> Arizona, Tucson, AZ.<br />

Reichhardt, K. 1992. Natural vegetation <strong>of</strong> <strong>Casa</strong> <strong>Grande</strong> <strong>Ruins</strong> <strong>National</strong><br />

<strong>Monument</strong>, Arizona. Cooperative <strong>National</strong> Park Resources Studies<br />

Unit. Technical Report <strong>NPS</strong>/WRUA/NRTR-92/45.<br />

10 Educational use only; not for sale

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