FOSSILS
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![]() Leaf and Insect Fossils from Florissant, Colorado Lower Oligocene 35,000,000 Years ago |
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The following information is copied from the website of the Proctor Museum of Natural Science with permission.
WHAT ARE FOSSILS?
Fossils are the evidence of things which
lived long ago. Fossilization or petrification
can be accomplished by various means. Some
things we call fossils are actually almost
identical to their status while alive, such
as many fossil shells. Usually fossilification
is a process where certain minerals replace
the fossil's original material. A good example
is petrified wood. The wood is replaced,
cell by cell, with minerals which may be
silicon and other minerals, to give the petrified
wood the beautiful colors which it often
has. It may also become opalized. Some fossilification
is by drying, such as mummified things in
desert areas. Some fossilization is done
in regions which are anaerobic, which means
there is no oxygen to aid in the deterioration
of the item. Some fossils are entombed in
amber and remain essentially just as they
were before being trapped and entombed. Therefore
fossil is a generic term for things which
have been preserved for long periods of time,
by many means.
WHERE CAN YOU FIND FOSSILS?
The answer is, almost anywhere that there
is a sedimentary formation. A sedimentary
formation is a layer of the Earth's cover
which accumulated over time. It may be dirt,
mud, debris which may form shale, then slate
in time; it may be shells and other calcereous
(i.e. CaCO3 or calcium carbonate) living
things or silicon, and other living things,
which may form limestone and marble; or plants,
trees other Plant Kingdom living things,
to make peat and coal. These layers gradually
build up by the action of wind, water, and
other means. Most sedimentary formations
are in horizontal layers (except where the
action of the Earth's crust has thrust them
upward or diagonally).
HOW LONG DOES IT TAKE TO MAKE A FOSSIL?
That is like asking how long is a piece of
string. Fossilification can be fairly rapid
or it may be hundreds of millions of years
and still not be fully fossilized. A good
example is when your PMNS Curator digs at
Florissant, Colorado which is lower Oligocene
fossils (approx. 35,000,000). While you find
fossil leaves and insects, where the item
is now a carbon residue, you can find pieces
of wood in the same matrix which crumbles,
but appears to still be pretty much wood.
For more information on how to tell the age
of formations, and hence fossils in those
formations.
, please
You may want to read Terry Proctor's award-winning article "Showing your Age" which appeared in the "BackBenders Gazette" on how to tell the age of specimens. Go to http://www.proctormuseum.us, click on Master Index, then click on Articles and then on"Showing your Age". This and other award-winning articles are available on this web site on the Articles page.
For more on fossils, go to http://www.proctormuseum.us, click on Master Index, then click on Fossils.
This site is still under construction. Thank
you for your patience.
Copy below here is for use in adding other
items which were on the previous website.
#1 Annularia radiata fossil leaves (Pennsylvanian era--310MYBP) from Tulsa County, Oklahoma (NEED TO FIND AND ADD PIX)
#2 Mastodon Tooth (Pleistocene era)--from Florida
#3 Eurypterid lacustrus (Sea Scorpion) (Silurian era) from New York
#4 Conus Shell (Middle Eocene era) from Burleson County, Texas
#5 Oreodont (Oligocene) a browsing animal about the size of a collie or sheep from Harrison, Nebraska
#6 Fossil Fern Plate #7 (Pennsylvanian era 310MYBP) from Tulsa County, Oklahoma (NEED TO FIND AND ADD PIX )
#7 Fossil Fern Plate #7 (Pennsylvanian era 310MYBP) from Tulsa County, Oklahoma
#8 Lepidodendron tree root (Pennsylvanian era--310MYBP) from Tulsa County, Oklahoma
This is the copy to the right hand side of
the Page:
The PROCTOR MUSEUM OF NATURAL SCIENCE, of
which I have been Curator for 15 years NOW
has their website online.
The PMNS website is http://www.proctormuseum.us.
Please visit this site and you will be amazed
at the amount of natural scientific material,
including fossils, shells, insects, articles,
biographies, places and trips and much more.
FOSSIL, GEM & MINERAL COLLECTING
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
Trips are being planned on the PMNS website
under "Places and Trips" and then
click on "Upcoming Trips".
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
DIGGING
Fossil collecting & Paleontology have
become more popular in recent years with
the finding of more dinosaurs and Jurassic
Park. Paleontologist Robert Bakker, PhD was
a consultant on Jurassic Park.
Dr. Proctor had the privilege of digging
dinosaurs with Dr. Bakker for a week in August,
1994. The dig was in the famous Como Bluff
area of Wyoming. Dr. Proctor learned a great
deal about getting dinosaur bones out of
the ground from Dr. Bakker.
For the past 15 years Dr. Proctor has been
Curator and Board Chairman of the Proctor
Museum of Natural Science. He has also been
Chairman of the Paleo Section of the Houston
Gem & Mineral Society and was twice the
Vice-President of HGMS and also Show Chairman.
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
Rockhounding is great and healthy exercise
but more than that it gives one an immense
sense of the enormity of God's creation.
From the most simple life form to the the
huge whales and dinosaurs, some form of life
has existed on this planet for most of the
4,600,000,000 years since this planet was
created.
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
eART SCANS OF FOSSILS & MINERALS
Some folks like to hang Paleontological and
Natural History type art work in their homes
and office. Terry Woodbeck, CEO of the new
Tulsa Spine Hospital chose the double-matted,
beautifully framed, Eocene Conus Shell with
the "contours" effect to hang in
that new hospital when it opens. You may
want to consider joining a "Rock Hound"
Club in your area and get out in the fresh
air and dig up some history yourself.
There is a larger picture of a Florissant,
Colorado mosquito (which is stored)
Here is the copy:
Fossil Mosquito (early Oligocene 35MYBP)
Florissant, Colorado