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Dear Jawod: <[EMAIL PROTECTED]> wrote in message news:[EMAIL PROTECTED] > Again, an amateur request for help. > > Can someone steer me in the right direction to determine the age of a layer > of limestone in a creek-cut hillside in my backyard? > > Being in Cincinnati, I know I am near (but not too near) the Cincinnati Arch > of Ordovician layers. Your thinking is obviously systematic. I think you can do the required sleuthing on your own if that is a prospect which interests you. I would use a search engine to check for geological maps on line along with information on the paleontology of the area. Derived from your own writing, some terms you may want to mix in the search would be +geology +"geological map" +paleontology +fossils +Cincinnati +"Cincinnati Arch" +"*** Ohio, etcetera. The asterisks would equal the sectional compass area of Ohio you are in. > I don't know the fossils very well. Shimer and Shrock are famous for their work "Index Fossils of North America". See your search engine, library or Amazon at www.amazon.com/exec/obidos/tg/detail/-/026219001X?v=glance for more details. An index fossil is generally a species which existed for only a small interval of geological time but occurs across an ample geographical area. Index fossils are accordingly great indicators of the age of the host rock, assuming they have not been reworked (redeposited) into sediments of a later time period. >This particular > formation is about 15-20 cm thick and lies between much thicker layers of > soft clayey shale of medium gray with very few fossils. This is in a > drainage area to the Little Miami River maybe ten miles north of its mouth > on the Ohio. I am thinking it is much less old than 450 MYA...but how much? The Ordovician Richmond Formation is plentiful in your area and sounds very close to what you describe. You will find a good bit on it online. > I am guessing that for most of the period while this rock was laid down was > turbid and muddy: the clayey shale. There was a period of clear water with > a prolific marine environment: the high density of shell debris and other > fossils in the limestone. Am I close? High energy deposition or turbidity is usually associated with a lot of broken fossils. Is that what you see? Taphonomy is the study of conditions and processes relating to fossilization---another search word for your pursuit. > The coolest thing, though, is that the under-surface of a large rock I > pulled out of its position in the cut has these great casts of indented > trails made by some crawling thing ...how long ago? So, I am thinking that > these trails occurred at the transition from a muddy swamp or something to a > clear water environment at that time. I'd have to see the specimen to join in your verdict. Carefully examine both sides of any broken rock face to make sure there are no hard fossil structures in one making imprints in another. Fossil impressions are called trace fossils or ichnofossils. There are a number of different trilobite impressions made by digging, walking, nesting, etcetera and there are known occurences of these in similar sediments from your area. Try looking at Google or Dogpile for images of cruziana(trilobite trackways) and rusophycus (trilobite resting places) to start. Here is a starter page on ichnology: http://www.geo.arizona.edu/geo3xx/geo308_fall2002/backup/cha3.html > What is the best approach to solve this puzzle? I suppose I could lug the > rock down to the Univ of Cincinnati Geology Department...what would they ask > me regarding the original location? anything else I should tell them? > > Thanks very much for understanding my enthusiasm and for looking past the > lack of training! I think you will have little trouble effectively pursuing this if you take a little time. The web is replete with sources for you. The U of C is heavily involved with area paleontology. It is the consensus choice in your area for institutional resources. There is also an amateur fossil club with a good reputation in the vicinity called the "Dry Dredgers". A number of knowledgeable folk belong who would be of aid to your quest. Jo made other fine suggestions for you to consider. Good luck and regards, Edward Hennessey nohalozzyzxnohalo.noyahoo.com minus no,no,no.
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