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Our new Biological Assessment is out - Klamath Basin Crisis

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<strong>Klamath</strong> Project Operations <strong>Biological</strong> <strong>Assessment</strong><br />

Endangered Suckers: Environmental Baseline for Suckers<br />

Table 2-4. Wetlands adjacent to UKL converted to agricultural land. Approximately<br />

8,000 acres, primarily in the Wood River watershed, were converted but are not<br />

accounted for in th<strong>is</strong> table.<br />

Site<br />

Acres<br />

Date<br />

Converted<br />

Acres<br />

(cumulative)<br />

Percent<br />

(cumulative)<br />

Wilson Marsh 100 1889 100 0.1<br />

Little Wocus Marsh 260 1889 360 1.3<br />

Big Wocus Marsh 3,800 1896 4,160 15.7<br />

Algoma Marsh 1,200 1914 6,660 25.1<br />

Caledonia Marsh 2,500 1916 7,860 29.6<br />

Hanks Marsh (Cove Point) 1,000 1919-40 8,860 33.3<br />

Ball Bay S<strong>out</strong>h 800 1919 9,660 36.3<br />

Williamson River Marsh 6,400 1920 16,060 60.4<br />

Wood River Ranch 2,900 1940-57 18,960 71.4<br />

Ball Bay West 410 1946-47 19,370 72.9<br />

Agency Lake North 2,600 1962 21,970 82.7<br />

Agency Lake West 4,600 1968-71 26,570 100<br />

Source: Adapted from Snyder and Morace 1997.<br />

Sedimentation Due to Watershed Alterations in UKL<br />

Sediment studies in UKL indicate a change in sediment composition and a<br />

substantial increase in sediment accumulation rates and nutrient concentrations<br />

over the last 150 years corresponding with increases in erosion input from the<br />

watershed (Eilers et al. 2001; Eilers et al. 2004; Bradbury et al. 2004). The<br />

changes in sediment composition and accumulation rates are cons<strong>is</strong>tent with land<br />

use activities that occurred during th<strong>is</strong> period, including substantial deforestation,<br />

drainage of wetlands, and agricultural activities associated with livestock and<br />

irrigation (Eilers et al. 2001; Eilers et al. 2004; Bradbury et al. 2004). Sediment<br />

accumulation rates have increased from ab<strong>out</strong> 18 grams per square meter per year<br />

(g/m2/year) in 1880 to a high of 120 g/m2/year in 1995 (Table 2-5). Eilers et al.<br />

(2004) and Bradbury et al. (2004) also found increases in sediment accumulation<br />

rates in UKL since the onset of development in the Upper <strong>Klamath</strong> watershed.<br />

69

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