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LIFELIKE PRESERVED CRETACEOUS PETRIFIED METASEQUOIA WOOD
WITH DRUSY CRYSTALS FROM HELL CREEK
Hell Creek Formation - Eastern Montana, U.S.A.
LATE
CRETACEOUS
PERIOD: 70 - 65 million years ago
Petrified wood in its natural form is less prevalent on the market
compared to sliced and polished examples. Unfortunately, when such
modifications are done to the specimen, the fossil value of the wood is
lessened and the piece becomes more of a pretty mineral showpiece rather than an
educational and intriguing
display fossil because the natural interior and exterior appearance
has been modified or in some cases, destroyed. On our recent 2005 field
collecting expedition to the Hell Creek Formation in Montana, we
collected and brought back only a few select pieces of petrified wood
from the Metasequoia tree. The METASEQUOIA was the
predominant tree that made up the Cretaceous forests where dinosaurs
such as Tyrannosaurus rex, Triceratops and various raptors lurked.
Holding a piece of this wood in your hand lets you actually feel the
texture of what this forest was like over 65 million years ago during
this final age of the dinosaurs! This petrified wood fossil is
perfect to display alongside dinosaur (or other life-forms) fossils such
as teeth and claws from Hell Creek and would greatly enhance the
educational value of any collection!
This specific Cretaceous
specimen displays rare features that are less commonly seen in your
typical petrified wood. The unique petrification process has retained the
most minute cellular structures, COLOR and texture of modern wood. This piece was dug so it had not been yet exposed to
the harsh elements of the Montana badlands. A seam of beautiful
drusy crystal chalcedony lines a portion of this strip.
NO REPAIR, POLISHING, OR
RESTORATION.
It is deceptively natural
looking and would make a superb display specimen of Cretaceous wood as
well as an enjoyable piece to handle with all its intriguing natural
texture and heavy weight!
The
Metasequoia tree that once grew in what is now the Hell Creek
Formation during the Cretaceous Period over 65 million years ago has
been closely compared to a living species found in China called
Metasequoia
glyptostroboides,
also known as the Dawn Redwood. This tree is a true living fossil
and was just discovered in a remote valley in Central China in the
1940's.
Back
during Cretaceous, the region where the Hell Creek Formation now is, was
once a region of meandering rivers, swamps and forested
floodplains. The temperature was subtropical to temperate much
like present-day Florida with a landscape similar to Florida in
appearance from the grasslands to the swamps. Metasequoia
trees dominated the landscape with trunks up to 12 feet in diameter and
over 100 feet tall. These trees produced small pinecones like the
present-day Metasequoia
glyptostroboides.
Petrified trees,
stumps, and logs can be found in the Paleocene Period deposits as well
as the older Cretaceous Period ones in Hell Creek. The petrified
wood can be found as stumps that still stand upright where they once
grew, as well as entire logs laying exposed with scattered limbs and
fragments. Despite the quantity that can sometimes occur, much of
it resembles simple rock. Fine natural display specimens that
resemble modern wood are fewer in numbers and are prized for their whole
life-like appearance when discovered.
Petrified wood forms when real wood lies buried underground and its
organic structure is gradually replaced with hard mineral. This
petrification requires rapid burial of the wood to prevent normal decay.
This can happen in different ways. A flooding river can have bury
the forest floor under a layer of sand and silt, for example.
Another circumstance could occur when forests are covered by volcanic
ash. After burial, mineralized groundwater begins to percolate
through the wood, coating cell walls and filling the intercellular
cavities with stone. In some cases, the entire log is converted to
stone and is solid like a cast of the original piece. In other
cases, the delicate cellular structures are preserved along with growth
rings, bark and knots such that the petrified wood exactly resembles
modern wood yet is heavy as stone when held, and clinks like porcelain.
Such detailed preservation is possible because the organic wood
molecules become coated and surrounded with smaller silica molecules.
Small amounts of impurities in the mineralized water add color to the
fossilized wood. The hues of yellow, brown and red indicate iron
while black and purple are derived from carbon or manganese.
A RARE EXAMPLE OF REALISTIC-LOOKING
PETRIFIED WOOD FROM THE CRETACEOUS HELL CREEK FORMATION!
6.7" long
SOLD PL-019
Actual Item - One Only |