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Old John Thomas was quite a character in his own right, but the
range was named long before Mr. Thomas ever laid eyes on Fish Springs.
Back in 1859 when Captain James H. Simpson topped out on Dugway
Pass while exploring for a new wagon road from Camp Floyd to Carson
Valley, he stated the following concerning the range in his official
report "My party moved at a quarter to six. Course nearly southwest
across desert (altitude above the sea 4,370 feet), thinly covered
with short Artemisia or sage, to "Short-Cut Pass" altitude
above the sea 5,347 feet, in a mountain range which I call Colonel
Thomas's range after Lieutenant Colonel Lorenzo Thomas, Assistant
Adjutant of the Army." Back in the old days, Dugway Pass which
separates the Dugway range in the north from the Thomas Range in
the south was known as "Short-Cut" pass because it allowed
travelers to save the approximately 25 miles that it would take
to go around the range to the north or south.
The Thomas range
has some really fascinating geology and some very interesting mineral
deposits which have been and continue to be exploited commercially.
This area is a rockhounder's dream if you know what you are looking
at and looking for. Some of the different minerals found here include
beryllium, fluorspar, manganese, uranium, garnet, beryl, bixbyite,
and of course topaz. Back in the 1980's a book written by Dr. William
Lee Stokes entitled "Geology of Utah" was published by
the Utah Museum of Natural History, University of Utah. This book
makes a wonderful addition to any Utah explorer's library. In it
Dr. Stokes describes how the grotesque, tortured, rhyolite mountains
in the Thomas Range were created. He stated that when the volcanic
eruptions in the Thomas range occurred millions of years ago, the
lava behaved very differently than normal basaltic flows. According
to Dr. Stokes, rhyolite is composed largely of silica, nearly 75%
in fact. This caused the flows to be more viscous and instead of
flowing in rivers of molten rock like in Hawaii, this lava spewed
out and piled up upon itself which explains the mud cake mountain
appearance of Topaz Mountain and many other peaks in the range.
The forces of wind, water, sand, and ice have eroded the ancient
rhyolites into otherworldly shapes that would make Carl Sagan proud.
These rocks are also very sharp and abrasive. They will chew up
your shoes in short order and will mangle your hands if you slip
and try to catch yourself so good leather boots and gloves are a
good idea if you are going to do some climbing in this range.
On one particular
visit, I climbed almost straight up the rhyolite to the summit of
peak 6,408 which is immediately south east of Topaz Mountain. This
peak forms the eastern wall of the Topaz amphitheatre. The funny
thing about this trip is that when I reached the summit, I tried
to pull myself up on top and I reached completely over the top to
the other side. I was stuck clinging to a knife ridge. My older
brother didn't appreciate this predicament at all and getting him
down was like coaxing a mule that didn't want to go one step further.
It is also interesting to note that the world's largest known deposit
of Beryllium is located in the Thomas Range at Spor Mountain. Beryllium
is a high strength, light weight metal which is used for military,
aerospace, and medical applications. The Brush Wellman Company exploits
this deposit and if you go to their website at www.brushwellman.com
you can find out all kinds of interesting information.
There are several
intriguing legends about this range and its riches. The best one
is probably nothing more than a fish story but it fires the imagination.
It is found in George A. Thompson's book "Some Dreams Die -
Utah Ghost Towns and Lost Treasures". In this book, Mr. Thompson
relates the story of the lost Crystal Cave. In this story, a professor
from California was prospecting in the northern part of the Thomas
range on a rainy blustery day nearly 60 years ago. As this man was
walking along, he stepped on the rhyolite crust and it broke away
and he crashed down into a subterranean chamber. He stated that
he had fallen into what he described as a giant "Geode",
the walls of which were covered with beautifully colored, perfect
topaz crystals. As it seems is the case in all of these stories,
he made off with as much as he could carry but he was never able
to find the cave again after that time. There are certainly lava
tubes and caves in the basalt flows near Fillmore and in the famous
El Malpais or badlands of New Mexico so it is at least possible
in theory but I am extremely skeptical. Could make a fun outing
to go and look for it though as you are sure to find smaller Topaz
crystals lying about.
What is Topaz
anyway? Topaz is a fairly common gemstone that has been used in
jewelry for centuries. The Egyptians said that Topaz was colored
with the golden glow of the mighty sun god Ra. The Romans associated
Topaz with Jupiter, who they also believed was the god of the Sun.
It occurs in the Utah desert as crystals approximately 1/8 to ½
inches long. Topaz is a prismatic crystal that tends to have a high
luster. It occurs in many different colors including clear, yellow,
orange, red, blue, and green. Most of the Topaz crystals found in
the Thomas Range are naturally amber but when exposed to sunlight
for long periods of time, become colorless or clear.
Topaz is the
November birthstone and it is also one of the hardest minerals in
nature. Topaz is also the State Gemstone of Utah. The crystals at
Topaz Mountain formed within cavities of Rhyolyte, a volcanic rock
that erupted in the area approximately 6 million years ago. Gathering
specimens at Topaz Mountain is quite easy. I have visited the area
several times and each time I have come away with some splendid
crystals. They are not very large but the clarity is startling.
They make you think to yourself "Hey, I've really found something
here" and that's a cool feeling when you go exploring.
Getting to Topaz
Mountain is not so easy. If you approach from the Delta area, you
can follow the paved "Brush-Wellman" road to within 3
miles of the collecting area which makes the mountain very accessible
to that community. To get to the Brush Wellman Road which is actually
Utah Highway 174, follow Utah Highway 36 south out of Tooele approximately
50 miles to Tintic Junction. At this point turn right onto U.S.
Highway 6 and follow it for 37 miles through the tiny town of Lynndyl
(remember that word for your next scrabble game when you're stuck
with all the junky letters) and turn right at the junction with
Highway 174. From here you simply follow the paved road all the
way out to Topaz Mountain and at that point follow the signs to
the collecting areas.
An altogether
different, more interesting route is to follow the old Pony Express
Trail out into the area. To get there, follow the Pony Express trail
through Government Creek, Past Simpson Springs, across the Old River
Bed, and finally to the vertical pump house and trough of the Topaz
Well. Make sure that you visit the Pony Express station monuments
and ponder the past along this route. At Topaz Well, turn left or
south and follow this road about 15.9 miles to the junction with
the Weiss Highway which is an improved dirt road that connects Jehrico
to Callao. Turn right or west on this road and follow it for about
2 miles and you will see a sign that says "Topaz Mountain Rock
hounding Area". Turn right on this road and follow it to the
large white colored mountain before you which is Topaz Mountain.
To find the
Topaz Crystals, you can go just about anywhere on the mountain.
I have had the best luck in what is called the Topaz Mountain Amphitheatre
which is a natural bowl or box canyon that the road goes into if
you follow the described route. Near the end of this road, I look
for crystals in the sand and gravel of the bottom of the main wash.
This is an easy place to find the crystals but it is also the most
worked over. You can climb all over the mountain and find crystals
eroding out of the Rhyolite.
If you plan
on going to Topaz Mountain, take plenty of water, make sure you
have a spare tire and the means to change it, food, first aid kit,
and a full tank of gas. Cell phones don't work out in the desert
so take what ever you will need and be prepared. Respect the gravel
roads and don't travel too fast or you will loose control of your
vehicle and it could be very ugly. Winter is an excellent time to
visit the Thomas Range because these mountains receive very little
snow and the temperatures on average are warm enough to do some
rock hounding in relative comfort. Lastly, if you are not familiar
with the Desert, make sure that you are not caught on the unfamiliar
roads after dark because it is very easy to get lost out there.
Visiting Topaz Mountain and the Thomas Range can be quite an adventure,
but it is worth the effort if rock hounding is an interest that
you have.
For more information
contact the Salt Lake City BLM District at 801-977-4300 or 801-539-4300.
http://www.ut.blm.gov/saltlake_fo/
Copyright ©
2008 Jaromy D. Jessop - All Rights Reserved
Reprinted with permission - Jaromy
D. Jessop
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