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Image Title Description Date
Fitts Park encircling creek 3  Abundant water in the park creates habitat for waterfowl.
 
2008-05-13
 
Fitts Park encircling creek 4  The diverted stream flow re-enters Mill Creek at the west end of the park.
 
2008-05-13
 
Fitts Park channel  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
 
Landscaping  A new real estate development in an old neighborhood uses the adjacent stream for its common landscaping.
 
2008-05-13
 
Mill Creek at 9th West  The last two miles of the Mill Creek streambed have been channelized before the stream enters the Jordan River.
 
2008-05-05
 
Central Valley Reclamation  The Central Valley Water Reclamation facility discharges water into Mill Creek about a mile before the stream enters the Jordan River.
 
2008-05-05
 
Lower Mill Creek  Stream velocity slows as the streambed gradient flattens near the Jordan River.
 
2008-05-05
 
Mill Creek outlet at Jordan River  Mill Creek enters the Jordan River at approximately 2900 South.
 
2009-11-06
 
Drainage looking north from Lone Peak  Bells Canyon Creek, sometimes called North Fork of Dry Creek, was formed by glaciation.
 
1995-09-11
 
Rivulet pool  A rivulet coming off Lone Peak creates a small pool.
 
1997-10-15
 
Lower falls  The lower falls are one of two waterfalls on Bells Creek.
 
1991-10-02
 
Silver Lake  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
 
Snowmobilers  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
 
Snowshoers  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
 
Inside a snow slide  Inside a remnant snow slide in Silver Fork.
 
1980-08-04
 
Fisher  Reynolds Flat, where the streambed gradient almost flattens, is a popular place for fishers.
 
2009-08-24
 
Reynolds Peak  Reynolds Peak at the top of Mill D North Fork is near the divide between Big Cottonwood and Mill Creek drainages.
 
2008-02-09
 
Doughnut Falls  Doughnut Falls in the Cardiff Fork drainage is a popular hiking destination.
 
2008-10-31
 
Mt. Millicent  Mt. Millicent is part of the Brighton Bowl at the top of Big Cottonwood Canyon. Late spring and early summer snowmelt provides approximately 50% of the flow in Wasatch Front streams. The rest comes from residual melting, rain and groundwater that seeps into the streambeds.
 
2008-02-29
 
Cardiff Fork debris  In autumn when streamflows diminish, tributary creeks can appear placid. Yet remnant debris signals the ferocity of falling water in late spring and early summer.
 
2008-10-31
 
Cardiff Fork in autumn  Like many tributary drainages in Big Cottonwood Canyon, Cardiff Fork once was the location of feverish prospecting for precious metals.
 
2008-10-31
 
Cross-country skiers  Cross-country skiers work their way up Mill D North Fork to Dog Lake. At the top of the drainage, they can drop into Big Water drainage and ski down Mill Creek Canyon.
 
1984-02-12
 
Reynolds Flat  Three drainages empty into Reynolds Flat Mill D South Fork (Cardiff Fork), Mill D North Fork and Days Fork. The open area provides space for two popular Forest Service campgrounds: Spruces and Jordan Pines.
 
2008-10-31
 
Butler Fork  Two small creeks converge to form Butler Fork on the north side of Big Cottonwood Canyon. Hikers often spot moose in the well watered drainage.
 
2007-09-25
 
Argenta dam site  Water developers once called for a dam and reservoir at Argenta. Storing 12,000 acre-feet of water and covering 143 acres, the lake would have stretched back 1.25 miles to Cardiff Fork. The plan was voted down in a bond election after the Utah Society of Engineers came out against it.
 
2008-10-31
 
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