home
***
CD-ROM
|
disk
|
FTP
|
other
***
search
/
Merciful 1
/
Merciful - Disc 1.iso
/
software
/
p
/
portal
/
portal3.dms
/
portal3.adf
/
t213
< prev
next >
Wrap
Text File
|
1986-10-29
|
2KB
|
62 lines
HISTORICAL-CULTURAL Datalink Entry:
TERMINUS-SOREL REPORT SUMMARY
Record of Third Transantarctic Safari,
January 15, 2012. Sunday. The weather
has been favorable, with continuous
sunlight, occasional high thin clouds
and light winds. We have traversed a
stretch of sastrugi for the past four
"days," moving toward the Pole of
Relative Inaccessibility. Our twelve
all-terrain vehicles (crawlers) have
performed beautifully. The new
electrolytic refuelers have done well
also. Toward "noon," the lead ATV slid
sideways unexpectedly, and we had to
pull it out of a steep, though not deep,
crevasse. While the rescue operation was
under way, I decided to take a few days
for a circuit of the vicinity; I had
spotted what looked like an interesting
nunatak in the distance and wanted to do
some radioglacialogical soundings near
it, but as I approached it appeared to
recede. Even triangulation with laser
rangefinders produced ambiguous
instrument errors. After two hours my
own crawler slipped against a sastrugi
and stopped. It looked as if I would
have to stay here for a time, so I
secured tent and crawler and set out
instruments.
I had completed one pass of the ice when
a storm came up suddenly.
(Gap in the record.)
The sudden storm ended, and I am now
ready to return to the rest of the
Safari. I fear they will not believe me
when I tell them about Terminus.
(Gap in the record.)
...I found myself looking into an
impossible abyss. The sunlight caught
the tops of clouds below me, which
parted, and below I saw what seemed to
be a perfect dry valley underneath the
ice! I spent several hours attempting to
photograph this valley, which I have
named Terminus. Although the photographs
are of low resolution and nearly
useless, I personally swear that I could
see vegetation, a lake fed by what
appeared to be a river. I would assume
some form of volcanic warming to this
region, with the river and lake fed by
glacial melt.