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Subject: Hasenmayer and the Blautopf
To: cavers@ge*.co* (Cave Diving), techdiver@terra.net (Tech Diver)
Date: Tue, 5 Mar 1996 12:18:05 -0500 (EST)
From: Jim Wei <jwei@ci*.uf*.ed*>
My buddy Dave Scheer in Germany translated the following article from the
local newspaper about Hasenmayer.  

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X-Sun-Data-Name: Blautopf
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The Blautopf is a cave system in the Karst plane of the Schwabish Alps in 
the vicinity of Ulm Germany. These mountains are a front range for the 
Tyrolian Alps which lie approximatly 100 km further south. The cave system 
was formed in the typical manner by solution etching but with the added 
compliction that the karst was being curved by the intrusion of the Alps late 
in the formation. This resulted in a cave system that has it's deepest point 
very near the entrance and then it has large excursions in depth until at 
about 1300 m ( 3900 ft) the system emerges into a semi-dry area called the
Moerike Dom (Cathederal). The system extends beyond this and theoreticlly 
should increase in depth again and may or may not extend for considerable 
distances. The exploration of this system has been carried out mostly by 
one man, Jochen Hasenmayer who has been a leading cave explorer in Europe. 
He did some of the pushes in Wookey Hole and Swildon in England and for 
many years held the depth record at Vacluse in southen France. He is often 
reticent to talk about what he does and therefore his accomplishments aren't 
recognised until years later when other teams begin to push the limits such 
as was the case in Vacluse.

The Blautopf system itself presents some special problems as it lies in the 
village of Blaubeuren and hence entry is severely restricted. The water is 
around 9 deg C (50 deg F) and the flow ranges from what Little River is when 
the water level is low to a boiling 32 times that when the snow begins to 
melt in the Schwabish Alps. It can be penetrated with scooters or swimming 
when the flow is low but when the flow is above minumum, penetration is no
longer possible due to the high flow rates encountered in the "Dueze' 
(The Nozzle) a restriction near the entrance. At flow rates that occur on 
especially high snow melt years the flow increases to a point that most of 
the village is flooded and has to be evacuated.

Several years ago Jochen suffered a DCS hit when starting his decommpression 
schedule 20 m too shallow due to a faulty depth gauge. He lost the use of his
legs but recovered when taken to a chamber. Due to another error in the 
chamber he was again paralysed, this time permenantly. He now dives using what
can best be called a wheelchair for divers. He is wet from chest level down 
but the upper torso is enclosed in a plexiglas observation chamber that is 
equalised to the external pressure, hence it can not really be called a U-boat 
as the press wants to do. He still must go throught the normal decompression 
schedules but does have a dry area in which to eat or drink. He has claims 
of being able to maintain himself for up to 14 days. The power system is 
NiCad batteries with propelsion being provided by what looks like standard 
scooters attached to the support frame. All this work is done on his own 
time and with his own funds as he has a full time job with the local 
equivalent of our IRS.

His main stated objective is to 'prove' that the Blautopf cave system was 
formed before the karst plain was curved and hence there must be an extensive 
system of filled caves under the Alps that would contain suficient hot water 
to provide household heating for a considerable period of time, on the order 
of centuries. This theory is not very widely accepted as many geolgists place 
the time of formation of the Blautopf after the Alps intruded and hence there 
is no downstream section and no basin of hot water.  From the cave divers
viewpoint the cave itself is beautiful in that the water is chemically 
coloured to an azure blue by copper compounds leached out of the limestone. 
The wet part of the cave is not noteworthy but the cave emerges into several 
dry areas, the largest which has been discovered to date is the Moerike Dom. 
This dry area is over 100 ft high by 300 ft long and has beautiful 
speleothems that are to date, seen and photgraphed only by Hasanmayer. 

 
The following article was in the Stuttgart newspaper describing his weekend
dives:
*******************************************************************

Stuttgarter Zeitung
Suedwestumschau
5 March, 1996
Blaubeuren, Alb-Donau-Kreis.

The crippled cave researcher Jochen Hasenmayer has shown new information 
after his latest dives in his Mini-U-Boat "Speleonaut" in the Blautopf near
Blaubeuren. The 54 year old Pforzheimer said yesterday that he now 'knows'
that the cave is older than 250 thousand years. 'The information lies on 
the table' says Hasenmayer. 

[Ed: this is folowed by a picture of what would appear to be a stream bed 
formed during a dry period in the system thus indicating that the cave has 
to be old enough to have gone through a dry period in history, hence older 
than the 250 k years stated by some geologists]

We have exactly the photo we want to have, said the researcher. With this 
trip in his 2.5 m long, 72 cm wide U-boat into the biggest water source
cave in middle Europe Hasenmayer has found a dry stream bed. The Blautopf 
is the source for the some of the blue of the nearby flowing 'Blue Danube' 
(Donau). It is also his entrance to the underwater world beneath the Alps. 

This photo taken at a 32 m depth shows a sharply defined stream bed etched 
in the bottom of the cave. The 54 year old spoke of a 'geological sensation'. 
This seems to prove that the cave is over 250 million years old and was 
formed before or during the intrusion of young Alps.
 
This seems to prove his theory that there is a underground resorvoir of 
approximately 35,000 square kilometers of water which must be at a
temperature of over 125 deg C (250 deg f) available under the Alps to 
provide heating for south Germany for over a century.

Hasenmayer plans other excursions into the cave and by fall expects to 
prove unquestionably that the thermal resource exists.


-- 

/********************************/
/*   Jim Wei                    */
/*   jwei@ci*.uf*.ed*           */
/*   Dept. of Computer Science  */
/*   University of Florida      */
/********************************/


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