The Merced like many other southern High Sierra rivers and creeks that include as part of their drainage basins elevations above 11,000 feet, often have areas of permanent snow and or small glaciers. Our 7.5 minute USGS topographic maps of those higher elevations show a great many of those snow fields. Thus those snowfields may provide a source of minimum flows even after the driest periods like the drought of 1976/77. Although water tends to quickly drain off of the dominant Sierra granite geology, areas with considerable talus tend to seep out their water more slowly. In the Southern Sierra, the Kings River and San Joquin River often have the largest minimum late season fall flows even in droughty years because they have the most high elevation areas with permament snow areas.
And to the north of Yosemite where highest elevations tend to be quite a bit lower, there is often considerable volcanic geology that absorbs and releases water more slowly. Thus rivers like the Feather with its considerable volcanic areas always have significant late season flows.
In any case, there are a great many creeks and rivers in the Sierra that do dry up by mid fall every year and others that dry up only after droughty periods. In fact some of those rivers may be rather large during early summer. But if their basins do not source some of the above higher elevations or seeping geologies, they may dry up. ...David
Post Edited (07-14-07 23:22)
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