President's
Corner
Gerry Naugle
I would like to thank
Dennis Gertenbach and
Dr. Bruce Geller for
setting up a real nice
club field trip to the
CSM Geology Museum in
Golden on Feb 9th. We
had the largest
attendence ever for a
field trip and did get
to see the back-room
area of the Museum. Some
photos from that field
trip will appear later
in this newsletter.
We will have a
presentation by Dr. Kirk
Johnson, Vice President
of Research &
Collections and Chief
Curator of the Denver
Museum of Nature and
Science (DMNS) on [most
likely topic] The
Fossils of the Douglas
Pass area at our March
13th monthly club
meeting at the West
Boulder Senior Center,
start at 7:15pm.
Our April club meeting
(April 10) will be the
first of our two annual
Silent Auctions. I
encourage everyone in
the club to read the new
rules and procedures for
this event, and then
contact the 2008 Auction
coordinator, Mr. Bob
Smith. Details are in
the article.
Club meetings are held
in the West Boulder
Senior Center, 9th &
Arapaho, at 7:15 PM.
Members are encouraged
to bring specimens they
have found or lapidary
projects they have
completed to meetings.
Also, there are several
experts in the club who
can help you identify
that mystery mineral or
fossil you have found.
****************
Spring & Summer Meeting
Schedule
Besides the excellent
speaker for the March
meeting (see President’s
Corner above), Terry
O’Donnell has set up an
excellent series of
talks for our upcoming
spring and summer
meetings. Here is a
brief list, so you can
put these dates on your
calendar:
April 10 (see
President’s Corner
above), Silent Auction
May 8, Ed Raines on
Leadville, the EPA, and
Me (and Beyond)
June 12, Dr. Robert
Amerman on Undersea
Movements and their
Geologic After-effects
July (date to be
determined), A joint
meeting at the RAMs
claim????
August 23 (Saturday),
Our annual picnic, North
Boulder Park main
pavilion, 11:00 AM.
****************
Junior Geologists
Activities
The Jr. Geologists are
growing in leaps and
bounds, with seven new
members joining our
group this winter. We
want to welcome Charles
Mock, Alex and John
Dixon, Jacob and Megan
Little, Noah Barton, and
Nico Caballero into the
club.
This winter, the Jr.
Geologists have been
working on the Rocks and
Minerals badge. Twelve
juniors have completed
the requirements for
this badge, for which
they have learned about
the differences between
rocks and minerals;
identifying minerals
with an ID kit they
made; Colorado’s state
rock, mineral, and gem;
and how to grow
crystals. Several of the
crystals they grew are
quite beautiful.
Congratulations to all
of those who have earned
this badge.
We are now working on
the new Earth Processes
badge, where the juniors
are learning about
igneous, sedimentary,
and metamorphic rocks,
volcanoes, earthquakes,
and plate tectonics; and
the rock cycle. Once the
weather warms up, the
juniors will take a
field trip to collect
sedimentary, igneous,
and metamorphic rocks in
the area. And, we plan
some neat experiments to
demonstrate our dynamic
Earth. The next Jr.
Geologists meeting will
be Thursday, March 20 at
7 pm at Charlotte’s
house. Besides working
on the badges, each
month features a special
mineral of the month,
plus great give-aways.
The Jr. Geologists
program is open to all
Flatirons Mineral Club
families. We meet on the
third Thursday of each
month, plus have special
weekend activities from
time to time. For more
information about the
Jr. Geologists program,
please contact
Dennis Gertenbach or
Todd Shannon.
****************
Upcoming Field Trips
With springtime just
around the corner and
the weather getting
warmer, we have begun
scheduling club field
trips. Be sure to
contact the trip leaders
for trip details, and to
sign up for these trips.
March 29-30 (Saturday
and Sunday): Book
Cliffs, north of Grand
Junction to collect
barite, calcite, and
selenite. Todd Shannon
will be leading the club
to the Persigo Wash
site, a less visited
area containing
barite-calcite nodules.
Some hiking from the
parking area is
required.
Trip Leader:
Todd Shannon.
April 12 (Saturday):
North Table Mountain,
outside of Golden, to
collect zeolite minerals
and calcite. This
world-famous site is a
great trip for kids,
because everyone will
find nice specimens. The
club has a special-use
permit from Jefferson
County to collect
minerals for this trip.
A hike of a little more
than ½ mile, climbing
about 700 feet in
elevation, is required.
Snow day will be April
26.
Trip Leader:
Dennis Gertenbach.
May 24-26 (Memorial Day
Weekend): Wyoming to
collect Kemmerer fossil
fish, Wamsutter
turitella agate, and
perhaps Blue Forest
petrified wood. We will
visit one of the fossil
fish quarries (pay site)
to collect the fish you
see in all of the rock
shops. The turitella
agate is quite unique,
with fossil snail shells
in a hard agate, and can
be cut and polished.
Trip Leader:
Dennis Gertenbach.
Other Trips in the
Planning Stages
* McCoy to collect
Pennsylvanian age marine
and plant fossils
* Dotsero to collect
pseudomorphs of goethite
after pyrite and silica
after calcite
* Tepee Buttes, east of
Pueblo, to collect
Cretaceous marine
fossils
* Picketwire Canyon,
south of La Junta, to
visit the site of the
largest dinosaur
trackway in the US.
****************
2008 Silent Auction
Rules and Procedures
The FMC will have two
silent auctions per
year. This will: 1.
Allow everyone to
participate in selling.
2. Reduce the number of
tables to a manageable
number (limit number of
tables to those that
would fit in the meeting
room and eliminate the
overflow into the
adjoining rooms). 3.
Allow those members who
are working on the
auction time to also
bid. 4. Increase the
amount of money taken in
for the FMC. 5. Create
additional outside
interest in the club
that could result in
gaining new members.
The Silent Auction will
be held under the
following rules: a) One
table is for young
people only. b) One
table is for the club
only, as needed. c). The
rest of the tables are
divided into thirds. d)
Each person is allowed
to fill only one space
(on a table), and spaces
are assigned and marked
off with blue tape. e)
Applications for space
must be sent to
Bob Smith by e-mail
at (or) by USPS letter
to: Bob Smith, 5704 Rim
Rock Ct, Boulder, CO
80301 f) Verbal and
phone requests will not
be honored. g)
Applications must be
dated (e-mail date or
post marked) no later
than the day of the
monthly club meeting
that falls one month
before the silent
auction. h) Applications
must include the
following information:
Name, Address, Phone
number, E-mail address
(if available), Date
sent in, Are you a FMC
member (have paid dues
for this year)? i)
Spaces are allotted on a
first-come-first-serve
basis. j) After all
table spaces have been
filled, we will keep the
rest of the applications
and they will be put at
the front of the list
for the next silent
auction, if these people
apply again. k) All
applications are for the
cur-rent silent auction
only. Applications do
not carry over from one
auction to the next. l)
We will attempt to
notify all sellers who
have been awarded a
space at least 2 weeks
before the silent
auction by e-mail, if
available, or by phone.
It is the seller’s
obligation to notify the
Dealer Chair of any
changes in e-mail
address or phone number.
m) We will also attempt
to notify everyone who
applied too late to
participate in the
current silent auction
and to inform them that
they will be placed at
the front of the list
for the next silent
auction, if they apply.
They will also be first
in line for any no-show
spaces at the current
silent auction. n) Table
spaces will be held open
for those who are
assigned to those spaces
until 7P.M. on the night
of the auction. After
that time, no-show
spaces will become
available first to late
applicants, then to
anyone who did not
apply.
****************
Club Lapidary Equipment
The club owns a wide
range of lapidary
equipment that is set up
in Charlotte Morrison’s
basement and garage.
This equipment is
available for use by
club members on
Wednesday evenings or at
other times by
appointment. If you are
inexperienced, but want
to learn how to use the
equipment, Charlotte
will arrange for an
experienced member to
show you how to use the
equipment. Be sure to
call Charlotte and let
her know when you will
be coming.
****************
Field Trip to the CSM
Geology Museum
Over 40 club members
attended a special
insider’s tour of the
Colorado School of Mines
Geology Museum on
February 9, our first
field trip of the year.
Bruce Geller, the museum
director, gave the club
a great tour of the
museum displays, plus a
behind-the-scenes look
at the museum’s
collection that is not
open to the public.
Bruce also explained the
expanded role that the
museum is taking in
assisting researchers
from both Colorado and
elsewhere.
We want to thank Bruce
for the great tour!!
****************
Bring Your Field Trip
Finds
If you found some great
specimens at one of our
club field trips, or on
a trip of your own,
please bring them to the
next club meeting to
show others. Everyone
enjoys learning where to
collect specimens and
what can be found.
****************
Be a Field Trip Leader
Do you have a favorite place to go collecting that you would
like to share with club
members? Would you like
to explore a new place
with others in the
club? If so, consider
leading or co-leading a
trip for the club.
Leading a trip is pretty
simple, you just need to
select a place and date,
promote the trip and get
club members to sign up,
collect the liability
releases from
participants, and go out
and have a good time.
For more information
about leading a trip,
please contact
Dennis Gertenbach.
Remember, the more trip leaders we have, the more field
trips we can have this
year.
****************
Geology
in the News
Dennis Gertenbach
Once again, our erstwhile news maven, Dennis Gertenbach has
supplied us with a
number of very
interesting news items,
as follow:
GOLD – The
New Exhibit at the
Denver Museum
GOLD, the largest
collection of gold ever
exhibited, is at the
Denver Museum of Nature
& Science from February
15 to June 8, 2008. This
fabulous exhibit of over
600 geological specimens
and cultural objects is
organized by the
American Museum of
Natural History, with
additional specimens
from the Denver Museum’s
collection. It traces
the influence that this
yellow metal has had on
human development.
Included are more than
80 natural specimens,
including crystalline
gold and gold nuggets,
170 cultural objects,
400 coins and gold bars,
and a 300-square-foot
room with walls and
ceiling completely
covered in just three
ounces of gold leaf.
Pre-Columbian jewelry,
some of the first gold
coins, rare doubloons
from sunken Spanish
ships, an Oscar, a
Grammy, and an Emmy are
part of the exhibit.
Gold’s central place in
Colorado’s history is
also showcased. Gold
brought the first influx
of European settlers to
Colorado, and the
exhibit features some of
best of Colorado’s best
specimens, including
Tom’s Baby, the largest
single mass of
crystalline gold ever
found in Colorado and
the 114-pound
Summitville boulder
found in 1975, a
volcanic rock containing
more than 22 pounds of
crystalline gold. The
Campion gold collection,
donated to the Denver
Museum in 1900, will
display John Campion’s
crystalline gold
specimens from his mines
near Breckenridge.
GOLD shows how gold is
deposited in the Earth,
where it can be found,
how prospectors find it
today, and how engineers
recover it from the
rock. The history of
extracting gold from
ancient times to modern
mining operations is
discussed. The exhibit
also shows why this
metal is so important
today and how many of
todays technological
advances depend on
gold’s unique
properties.
For more information
about the exhibit, visit
the museum’s
website. GOLD is
presented in Denver by
Newmont Mining
Corporation, with major
support provided by
Wells Fargo.
Origin of Rubies and
Sapphires Determined
Mineral collectors and
gem cutters are quite
familiar with rubies and
sapphires, corundum or
aluminum oxide found in
a wide range of colors.
The various tints are
due to trace impurities:
titanium and iron for
the blue of the
sapphire, chromium and
vanadium for the red of
rubies. Although these
gems have been sought
for thousands of years,
the origin of many gem
deposits has been a
mystery for geologists
and a subject of much
debate. This is
especially true for
rubies and sapphires
found in alkaline
basalts, volcanic rocks
that most commercial
gems are extracted.
Geologists have known
that these gems formed
at extremely high
pressures and
temperatures deep within
the Earth. Rising magma
then brought them up to
the surface where
erosion liberated the
crystals from the rock
and accumulated them in
placer deposits. Because
the original rock has
been weathered away, it
is extremely difficult
to determine the origin
of these gems.
Researchers at the
University of
Antananarivo studied
well preserved specimens
of ruby-bearing rock
from Madagascar and
determined that the
original magma
originated in the
Earth’s mantle. This
discovery shows that the
rubies and sapphires in
the alkaline basalts
were formed at extremely
high pressures (30,000
psi) and temperatures
(2,000 oF), 35 miles
below the Earth’s
surface. These
researchers compared the
ratio of oxygen isotopes
in the rubies in the
Madagascar rock with
ratios in 150 rubies and
sapphires from
commercial basaltic
deposits from 13
countries, and found
them quite similar. This
indicates that all these
rubies and sapphires
were formed under
similar conditions, thus
originated from the
Earth’s mantle. The
chemical composition of
inclusions in gems from
these deposits also
point to a similar
origin.
Meteorite
Dates Lunar Volcanoes
Japanese scientists
studying a 30-pound
meteorite found in
Botswana have determined
that it originated from
a long-ago lunar
volcanic eruption.
Furthermore, the ratio
of uranium and lead
atoms in the rock's
phosphate minerals,
allowed the team to date
this eruption at
approximately 4.35
billion years ago.
The most-accepted theory
of the moon’s origin
begins with a collision
between the Earth and a
Mars-sized body about
4.5 billion years ago.
The resulting material
thrown into space
coalesced into the Moon.
This meteorite shows
that volcanoes were
erupting on the Moon’s
surface about 150
million years after its
formation. This implies
that the Moon’s surface
cooled quickly to form a
crust and that the
interior had separated
into a mantle and a
core.
The meteorite is
hundreds of millions of
years older than rocks
collected by the Apollo
astronauts. These
ancient rocks help
scientists to better
understand the early
solar system, including
the Earth, because the
Moon is the only place
where geologists can
find rocks formed during
the first 500 million
years of the solar
system. Rocks of that
age on Earth have long
disappeared, due to
erosion and other
geologic activity on our
planet.
Diamonds
from Outer Space
Not all diamonds found
on earth are the hard,
shiny gems we are all
familiar with. Carbonado
diamonds, found only in
Brazil and the Central
African Republic, are
dark and frothy, full of
small bubbles like
pumice. Gem diamonds are
formed at extremely high
temperatures and
pressures deep inside
the Earth and then are
carried to the Earth’s
surface by explosive
volcanoes. However, the
frothy nature of
carbonado diamonds could
not have formed deep
inside the Earth and
their origins have
puzzled geologists.
Stephen Haggerty, a
geologist at Florida
International
University, and his
colleagues analyzed the
chemical composition of
the carbonado diamonds
by bouncing infrared
light off polished
slivers. The resulting
chemical signatures did
not match those of
terrestrial hydrogen and
nitrogen, but closely
matched those found from
particles measured in
interstellar space.
These findings suggest
that carbonado diamonds
were created by an
exploding star and
delivered to Earth by an
asteroid billions of
years ago.
The age of these
diamonds has been dated
to between 2.6 billion
and 3.8 billion years
ago, a time when South
America and Africa were
joined together. This
would explain why these
diamonds have only been
found in these two
continents, thus are
probably from a single
asteroid impact. The
color variation of the
carbonado diamonds, from
black and gray to green
and even red, suggest
that they were likely
embedded within another
rock, and not just one
giant carbonado diamond.
The host rock has since
weathered away, leaving
the carbonado diamonds
behind.
Did a Comet Cause the
Great Flood?
Over 175 cultures have
flood myths, telling of
a catastrophic
inundation of the Earth.
Bruce Masse, an
environmental
archaeologist at Los
Alamos National
Laboratory, has
theorized that these
widespread flood myths
may have originated from
an actual flood caused
by a gigantic comet
crashing into the Indian
Ocean several thousand
years ago, nearly wiped
out all life on the
planet. Furthermore,
Masse and other
scientists have found
evidence of such a
collision.
Masse theorizes that
some 5,000 years ago, a
3-mile-wide ball of rock
and ice smashed into the
ocean off the coast of
Madagascar. This
injected plumes of
superheated water vapor
and aerosol particulates
into the atmosphere and
sent a series of
600-foot-high tsunamis
crashing against the
world’s coastlines.
Within hours, the heat
and moisture blasted
into the jet streams,
spawning gigantic
hurricanes across the
Earth. Additionally, the
impact sent tons of
material into the
atmosphere, plunging the
Earth into darkness.
Thus, the origin of the
great flood stories
found in almost all
cultures around the
world. The bible tells
of Noah’s ark enduring a
deluge for 40 days and
40 nights. In the
Gilgamesh Epic, the
Mesopotamian hero saw a
pillar of black smoke on
the horizon before the
sky went dark for a
week. Afterward, a
cyclone pummeled the
land and caused a
massive flood.
Indigenous South
American myths also tell
of a great flood.
According to Masse,
these stories all
describe what the
survivors of such an
impact would see.
Two flood myths helped
Masse pinpoint the date
of such an impact. The
Hindu flood myth
describes the alignment
of five planets, which
has happened only once
in the last 5,000 years.
A Chinese story mentions
a great flood that
occurred at the end of
the reign of Empress Nu
Wa. These led Masse to
date the impact on May
10, 2807 B.C.
Dallas Abbott of
Columbia University
searched for debris that
would have been left
from giant waves
generated by such an
impact. Specifically,
tsunamis of this
magnitude would leave
gigantic, wedge-shaped
sandy structures known
as chevrons. Because the
tsunami would have
dredged material from
the ocean floor, these
chevrons would contain
deep-ocean microfossils.
Dozens of chevrons can
be found along
shorelines and inland in
Africa and Asia. The
shape, size, and
location of these
chevrons suggest that
they resulted from an
impact in the ocean off
Madagascar. Melted
deep-ocean microfossils
have been found in these
chevrons, providing
additional evidence of a
cosmic impact. The
scientists plan to
perform carbon-14 dating
on the fossils to see if
they are indeed 5,000
years old.
Fossils in the News
Dinosaur Demise from
Insects? A new book,
What Bugged the
Dinosaurs? Insects,
Disease and Death in the
Cretaceous, by George
and Roberta Poinar,
theorizes that insects
took out the largest
land creatures the world
has ever known. Although
the large asteroid
impact and massive
volcanic flows took
place at the end of the
Cretaceous when the
dinosaurs became
extinct, paleontologists
have been puzzled with
the gradual decline and
disappearance of the
dinosaurs before the
asteroid impact and
volcanic eruptions at
the end of the
Cretaceous.
Fossil insects from this
time trapped in amber
show that insect species
were evolving and
flourishing in the warm
temperatures of the late
Cretaceous. These
insects would have
competed with dinosaurs
and other herbivores for
food. Insects also
played a key role in the
widespread proliferation
of flowering plants at
this time, which were
rapidly replacing the
seed ferns, cycads,
gingkoes and other
gymnosperms that
herbivore dinosaurs
relied on. Additionally,
biting insects may have
carried new diseases
that attacked the
dinosaurs. This triple
punch may have slowly
led to the decline of
the dinosaurs that
eventually finished them
off.
In the book, the Poinars
describe that during the
late Cretaceous, the
associations between
insects, microbes and
disease transmission
were just emerging. In
the gut of one biting
insect preserved in
amber from that time,
Poinar has found the
pathogen that causes
leishmania. Leishmania
is a serious disease
still found today, that
can infect both reptiles
and mammals. In another
biting insect from this
time, the researchers
discovered organisms
that cause a type of
malaria that infects
birds and lizards today.
Nematodes, trematodes,
and protozoa have been
found in dinosaur feces.
Today, many of these
intestinal parasites are
spread by insects.
The triple attack of
insects – loss of
traditional food,
competition for food,
and disease – along with
a changing environments,
asteroid impact, and
massive lava flows may
have lead to the end of
the dinosaurs.
Biological Explosion in
the Precambrian
Paleontologists have
recently uncovered
evidence for a sudden
proliferation of species
at least 30 million
years before the
Cambrian period. During
the Cambrian, most of
the major living groups
of animals emerged
during a short period of
time known as the
Cambrian Explosion
(between 542 million and
520 million years ago).
Researchers from the
Virginia Polytechnic
Institute and State
University in Blacksburg
have studied strange
fossils from Australia,
known as the Ediacara
biota. These
multicellular organisms
emerged about 575
million years ago. The
Ediacara organisms are
quite different from any
creatures found in
subsequent fossils. Many
resembled leaflike
fronds and have complex
shapes and forms. They
emerged abruptly over
about 25 million years
during the Avalon period
in the Precambrian and
the research team has
named this biological
proliferation of species
the Avalon Explosion.
During this time, the
earth saw a sudden
increase in the oxygen
level in the oceans.
Additionally, an ice age
was ending on the Earth
and the oceans were
warming. These changing
conditions may have
triggered the Avalon
Explosion. Why these
creatures vanished,
while the Cambrian
Explosion produced phyla
that still exist today,
is not known.
New Fish-Eating Dinosaur
Discovered Scientists
have discovered an
unusual dinosaur that
had a skull similar to a
fish-eating crocodile
and two huge hand claws
that may have been used
as grappling hooks to
lift fish from the
water. Using computer
modeling techniques,
Emily Rayfield at the
University of Bristol
reported that the skull
of this dinosaur bent
and stretched in the
same way as the skull of
the Indian fish-eating
gharial -- a crocodile
with long, narrow jaws.
Excavation of the
dinosaur found partially
digested fish scales and
teeth and a dinosaur
bone in the stomach
region of the animal,
providing further
evidence that the
dinosaur ate fish at
least some of the time.
The unusual skull of
Baryonyx walkeri is
quite long, with a
curved jaw similar to
large crocodiles and
alligators. It also had
stout conical teeth,
rather than the
blade-like teeth of
meat-eating dinosaurs,
plus a rosette of teeth
at the tip of the jaw,
similar to that found
today in slender-jawed
crocodiles. However, the
skull design is
different from
crocodiles, suggesting
that this design evolved
independently in
Baryonyx and crocodiles.
This dinosaur lived
during the early
Cretaceous, around 125
million years old, and
belongs to the family of
dinosaurs called
spinosaurs. The fossil
was discovered in
Surrey, England.
Did a Comet Wipe Out the
First Americans?
Archeological evidence
has shown that about
13,000 years ago, the
Clovis people wandered
North America, hunting
ground sloths, mammoths,
and other creatures.
However, both hunters
and prey mysteriously
vanished; the cause of
which is unknown. Now, a
team of scientists think
they know - a large
comet smashed into the
Earth just north of the
Great Lakes. This
explosion triggered a
1,000-year cold spell
that led to the demise
of both the Clovis
people and the large
animals they hunted.
Previous theories for
the disappearance of the
Clovis people, along
with 35 genera of
animals, included
climate change and
excessive hunting by
humans. Supporting this
new theory of a comet
impact is a thin layer
of black soil found at
more than 50 North
American sites. Within
this black layer are
grains containing
iridium, an element
thought to indicate
extraterrestrial
origins, and melted
charcoal, likely from
wide-spread forest fires
after the impact.
Although no crater has
been found, the
concentrations of these
indicators are highest
around the Great Lakes,
suggesting the location
of the impact. The lack
of an impact crater may
be due to the impact
being absorbed and/or
erased by the ice sheet
that covered the area at
this time or the comet
could have exploded
before hitting the
Earth.
Giant Dinosaur-Eating
Frog Researchers lead by
David Krause from the
New York Stony Brook
University have
discovered the remains
of the largest frog
every discovered.
Beelzebufo (Devil Toad),
found in Madagascar,
lived approximately 65
to 70 million years ago
in a semi-arid
environment and was
about the size of a
bowling ball. It also
had an unusual diet,
hunting lizards, small
mammals, and even
dinosaur hatchlings.
The fossils of
Beelzebufo are quite
similar to fossil frogs
from South America,
supporting the theory
that South America and
Africa, along with the
island of Madagascar,
were a single continent
at this time. Also,
scientists speculate
that Beelzebufo went
extinct at the same time
as the dinosaurs.
****************
Upcoming Events, Nearby
& Elsewhere
Wed., Mar. 19, Friends
of Dinosaur Ridge Annual
Meeting, Volunteer
Appreciation Dinner, and
(belated) Arthur Lakes
Birthday Party;
featuring Dr. Martin
Lockley explaining
"Tracks 101, How to
Identify a Dino Track".
At the Dino Ridge
Visitors Center, 6:30
p.m., 16831 W. Alameda
Parkway, Morrison.
Fri.-Sat.-Sun. Mar.
28-30, Gem and Mineral
Show sponsored by the
Fort Collins Rockhounds
Club, at Lincoln Center,
417 W. Magnolia St.,
Fort Collins; see
http://www.fortcollinsrockhounds.org/
for more info. Featuring
“Minerals of the
American West”.
Friday April 11, North
Jeffco Gem and Mineral
Club Silent Auction.
North Jeffco Community
Recreation Center, 6842
Wadsworth Blvd. Setup
begins at 5:30 pm;
Auction begins at 6:45
pm. Mineral specimens,
gems, jewelry, crafts,
equipment, and bake
sale. Free parking, free
admission, and free
refreshments. Public
invited. Sellers and
buyers welcome. For
addition information
call Ron Knoshaug at
303-423-2923 or email at
jrknoshaug@comcast.net.
Fri.-Sat.-Sun. April
25-26-27, Colorado
Mineral & Fossil Show.
Holiday Inn-Denver
Central, 4849 Bannock
St., Denver, CO 80216.
Hours: Fri. & Sat., 10
a.m.-6 p.m.; Sunday, 10
a.m.-5 p.m. ADMISSION
FREE, Parking free.
Annual spring show and
sale of minerals,
fossils, gems, jewelry,
beads, meteorites,
decorator items, and
lapidary supplies. More
than 70 local, national,
and international
vendors sell
nature-related items for
collectors and the
general public. This is
a fun event for the
whole family, from kids
to senior citizens, with
items for sale in every
price range. Retail and
wholesale buyers will
find great bargains for
their collections,
personal adornment, home
décor, and gifts.
Participating vendors
come from China, India,
Pakistan, Morocco,
Ethiopia, and Tibet.
Local miners and jewelry
artists will sell their
finds and creations.
WEBSITE:
www.mzexpos.com.
Sat-Sun, May 17-18, The
mineral collection of
Dick Holmes will go on
sale May 17, Sat., 8:00
- 4:00 and Sunday the
18th, noon to 4:00. Dick
was a miner and a mine
inspector, with a
collection spanning 1925
to 1986, and he was the
author (with M.B.
Kennedy) of "Mines and
Minerals of the Great
American Rift" (publ.
1983). There will be
over 1,500 specimens,
mostly Colorado
minerals, many from the
San Juan and Leadville
areas. Cash only; Rain
or Shine; no pre-sales.
2980 S. Vine Street,
Denver, 80210 (south of
Denver University).
There will be many
specimens under $100,
Perky boxes in various
sizes, and hand-size
minerals up to large
crystal plates. A
complete collection of
"The Mineralogical
Record" from the first
issue to 1989 is for
sale - inquire day of
sale for a viewing
appointment.
Contact daughter Judy
Holmes, 303-758-5547.
****************
Notices of Interest to
FMC Members
We Need Your Help
The American Federation
of Mineralogical
Societies has an ongoing
goal of having subjects
of interest appear on
U.S. commemorative
stamps. Currently we are
attempting to get
gemstones on stamps.
The 2003 United States
50 State Quarters
program features a
faceted gemstone on the
Arkansas 25-cent piece.
Collect these and also
support gemstones on
stamps too!
We need you to actively
support and promote the
project by sending
letters expressing your
interest to the USPS.
You do not have to be an
AFMS member to write.
Letters or petitions for
stamp subjects should be
sent to:
The Citizen’s Stamp
Advisory Committee
c/o Stamp Development
U.S. Postal Service
475 L’Enfant Plaza, SW,
Room 5670
Washington, DC
20260-2437
Rainbow Lattice
(Australia)
I have an amount of GOOD
Rainbow Lattice found at
Harts Ranges some years
ago. As you are aware
this is a rare stone to
be found in useable
pieces. There is
literally tons of this
material to be gathered
with little or no effort
but to find something
worthwhile takes a lot
of searching time and
effort. The lot I have
was found in a rock in a
vein of ball-like
deposits. Nothing large
but breaks into 4/ 20 ct
pieces. I would be
willing to forward
pieces to you on
approval and let you put
your price on them. I am
approaching 80 and can
no longer fossick and am
disposing of my
collection I have maybe
600+ carats of this
material in varying
grades.
Ken Cross.
AA Mineral Specimens
(Australia)
AA Mineral Specimens is
a web-based mineral
dealer specializing in
the supply of mineral
and gemstone specimens,
lapidary materials and
fossils. Current stock
can be viewed at
www.aamineralspecimens.com.
AA Mineral Specimens
circulates a weekly
newsletter to inform
subscribers of stock,
deals and items of
interest. As the
newsletter may be of
interest to you, we are
currently promoting the
newsletter by offering a
US$5,000 store credit as
a prize for one lucky
subscriber. Details of
the promotion are
available on AA Minerals
website.
You and your Club
members can subscribe to
our newsletter by going
to our website and
clicking on the ‘Join
our Mailing List’
button. For further
information contact
Susan Lafferty and Bruce
Myles.
****************
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Updated 3/6/08 |