Find's Treasure Forums

Welcome to Find's Treasure Forums, Guests!

You are viewing this forums as a guest which limits you to read only status.

Only registered members may post stories, questions, classifieds, reply to other posts, contact other members using built in messaging and use many other features found on these forums.

Why not register and join us today? It's free! (We don't share your email addresses with anyone.) We keep email addresses of our users to protect them and others from bad people posting things they shouldn't.

Click here to register!



Need Support Help?

Cannot log in?, click here to have new password emailed to you

Changed email? Forgot to update your account with new email address? Need assistance with something else?, click here to go to Find's Support Form and fill out the form.

My Latest Fossil Page

Inyo

New member
Just thought I'd let folks know that my latest fossils-related web page is Fossil Insects And Vertebrates On The Mojave Desert, California :

Visit two world-famous paleontologic localities situated on California's vast Mojave Desert. They're from what geologists call the middle Miocene Barstow Formation. And--they're 17 to 13.4 million years old.

One specific site within the Barstow Formation is without question among the most unusual fossil-bearing areas on earth. Not only does it yield many species of insects, but also lots of spiders, water mites, fairy shrimp, ostracods (a small bivalve crustacean) copepods (a minute crustacean often called Cyclops), cladocerans (tiny crustaceans commonly called "water fleas"), and even diatoms (a microscopic single-celled plant), as well--all of which can be dissolved whole and intact, in three-dimensional form, from their calcium carbonate (limestone) concretion encasings. It is one of only a handful of places on the planet where fossil insects can be removed without damage from their matrix.

A second geologic district in the Barstow Formation provides vertebrate paleontologists with one of the most significant terrestrial records of middle Miocene animal life in North America--a place rich with the remains of extinct horses, camels, pronghorns and proboscideans, among many other mammalian varieties. It is, in fact, the type locality for what geologists, paleontologists, and stratigraphers call the Barstovian Stage of the middle Miocene, roughly 16 to 12.5 million years old--an epochal stage of North American Cenozoic Land Mammal Biochronology with which all other time-correlated rocks in North America are compared.
 

GTzer

New member
WOW- what a site. I'll save this for when I get snowed in sometime. Other wise I'll become part of this chair.
Outstanding!
 
Top