[Geysers] Excelsior & GPS

[TSBryan at aol.com]

Depending on your "definition" of "high flow volume"... back in 1986, when  
Fantail was actively discharging rather great volumes of water, we looked 
for  and could see absolutely no change in activity or discharge by such 
nearby (yes,  across the river, but very near) features as Hillside and Seismic, 
nor in the  nearby springs on the Fantail side of the river. I'm sure there 
are other  examples.
 
Scott Bryan
 
 
In a message dated 9/28/2010 5:02:14 P.M. US Mountain Standard Time,  
brdavis at iusb.edu writes:

Second,  are there other examples of such high flow volume features with 
such  significantly different hydrostatic levels located this close to each 
other  (and what is that due to - very different hydraulic conductivities, 
i.e., one  has significantly greater hydraulic "friction" than the other)? 
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