2006
DOI: 10.5962/bhl.title.24324
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The Big Blackfoot River Fisheries restoration report for 2004 and 2005

Abstract: Exhibit I: Westslope cutthroat trout genetic sampling sites and results.

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Cited by 4 publications
(2 citation statements)
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“…Kleinschmidt Spring Creek, a spring creek tributary to the lower North Fork of the Blackfoot River, is located on the floor of the Blackfoot River valley in west-central Montana (Figure 1). Discharge in Kleinschmidt Creek ranges from a low of 0.26 m 3 /s during winter and spring to a high of about 0.42 m 3 /s during midsummer months (Pierce and Podner 2006). Although Kleinschmidt Creek receives basin-fed runoff upstream of stream kilometer (skm) 3.2, approximately 90% of summer stream flows are generated by groundwater inflows from an alluvial aquifer, most of which surfaces between skm 1.6 and 3.2 Pierce and Podner 2006).…”
Section: Study Areamentioning
confidence: 99%
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“…Kleinschmidt Spring Creek, a spring creek tributary to the lower North Fork of the Blackfoot River, is located on the floor of the Blackfoot River valley in west-central Montana (Figure 1). Discharge in Kleinschmidt Creek ranges from a low of 0.26 m 3 /s during winter and spring to a high of about 0.42 m 3 /s during midsummer months (Pierce and Podner 2006). Although Kleinschmidt Creek receives basin-fed runoff upstream of stream kilometer (skm) 3.2, approximately 90% of summer stream flows are generated by groundwater inflows from an alluvial aquifer, most of which surfaces between skm 1.6 and 3.2 Pierce and Podner 2006).…”
Section: Study Areamentioning
confidence: 99%
“…Discharge in Kleinschmidt Creek ranges from a low of 0.26 m 3 /s during winter and spring to a high of about 0.42 m 3 /s during midsummer months (Pierce and Podner 2006). Although Kleinschmidt Creek receives basin-fed runoff upstream of stream kilometer (skm) 3.2, approximately 90% of summer stream flows are generated by groundwater inflows from an alluvial aquifer, most of which surfaces between skm 1.6 and 3.2 Pierce and Podner 2006). To examine stream temperature reduction, we monitored stream temperatures in the North Fork of the Blackfoot River at U.S. Geological Survey (USGS) gauge station 12338300 and treated this as a control site in the study (Figure 1).…”
Section: Study Areamentioning
confidence: 99%