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flows seasonally, based on the water supply. In the summer and fall, freestone streams grow warm and have reduced flow because water from snow melt is less readily available. In contrast to limestone streams, which flow over
41:, and crystalline rocks. Additionally, freestone streams are supplied by runoff and snowmelt, while limestone streams are usually fed by springs, providing cooler waters and a more stable
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Water
Quality in the Lower Susquehanna River Basin, Pennsylvania and Maryland, 1992-95, U.S. Geological Survey Circular 1168
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Lindsey, Bruce D.; Kevin J. Breen; Michael D. Bilger; Robin A. Brightbill (1998).
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64:"A Trout Stream Top to Bottom"
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