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Date: Tue, 22 May 2001 08:10:13 -0700 (PDT)
From: terry michael <OEA51@go*.co*>
Subject: Re: Re: "reverse flow"
To: Christopher Brown <hokiediver@ya*.co*>, techdiver@aquanaut.com
Calcium carbonate remains (basically).


-----Original Message-----
From: "Christopher Brown"<hokiediver@ya*.co*>
To: techdiver@aquanaut.com
Date: Fri May 18 04:17:50 PDT 2001
Subject: Re: "reverse flow"

>What is a karst plain, anyway?
>
>Chris Brown (not a caver)
>Suffolk, VA
>
>--- Trey <trey@ne*.co*> wrote:
>> 
>> Blue holes are tidal but can have some very twisted
>> relationships to the
>> tides. Caves in karst plains tend to move in one
>> direction unless there is a
>> temporary disruption , like the breaking of an
>> aquaclude. Springs,
>> especially along rivers, can reverse and siphon when
>>  the level of the
>> surrounding water rises. Speed of flow is definitely
>> not only tidal ( moon
>> pull ) , but dependent upon the hydrostatic head
>> which can change locally,
>> or at a great distance, but is most likely to change
>> quickly locally, as in
>> low tide at a resurgence into the Gulf where the
>> head is coming from 50
>> miles away.
>> 
>> -----Original Message-----
>> From: Aldo P. Solari [APS]
>> [mailto:aldo.solari@ho*.se*]
>> Sent: Thursday, May 17, 2001 7:16 PM
>> To: techdiver@aquanaut.com
>> Subject: "reverse flow"
>> 
>> 
>> Dear senior technical divers,
>> 
>> I  wonder  whether  anyone  could  explain  the 
>> causes  of  the
>> phenomenon of "reverse flow" occurring in caves.
>> 
>> Does  the  "reverse  flow"  occur  due  changes  in 
>> atmospheric
>> pressure,  tides,  coreolli  forces,  venturi
>> effects through the
>> cave entrance or any other mechanism/s ?
>> 
>> An interesting topic.
>> 
>> Cheers,
>> 
>> aldo.solari@ho*.se*
>> www.ccbb.ulpgc.es/fish-ecology/solaris
>> ___
>> 
>> 
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>
>
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