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The diverted stream flow re-enters Mill Creek at the west end of the park.
2008-05-13
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The Mill Creek streambed has been channelized on the park's south side. Channelization accelerates water velocity and can cause streams to cut deeper into their beds, eroding them.
2008-05-13
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A new real estate development in an old neighborhood uses the adjacent stream for its common landscaping.
2008-05-13
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The last two miles of the Mill Creek streambed have been channelized before the stream enters the Jordan River.
2008-05-05
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The Central Valley Water Reclamation facility discharges water into Mill Creek about a mile before the stream enters the Jordan River.
2008-05-05
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Stream velocity slows as the streambed gradient flattens near the Jordan River.
2008-05-05
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Mill Creek enters the Jordan River at approximately 2900 South.
2009-11-06
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Bells Canyon Creek, sometimes called North Fork of Dry Creek, was formed by glaciation.
1995-09-11
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Silver Lake is a popular, year-round recreational spot. A boardwalk makes it wheelchair accessible in the summer. Cross-country skiers circle it in winter.
2009-08-11
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Snowmobilers sled on the Guardsman Pass Road. As Salt Lake Valley population soars, there are inevitable conflicts between incompatible uses of the watershed.
2008-02-29
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Snowshoers trek on the Guardsman Pass Road. As Salt Lake Valley population soars, there are inevitable conflicts between incompatible uses of the watershed.
2008-02-29
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Reynolds Flat, where the streambed gradient almost flattens, is a popular place for fishers.
2009-08-24
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Reynolds Peak at the top of Mill D North Fork is near the divide between Big Cottonwood and Mill Creek drainages.
2008-02-09
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