Tuesday, June 29, 2010
Protoleptostrophia perplana Brachiopod
Half of an internal Protoleptostrophia perplana (Conrad, 1839) brachiopod found in the Silver Creek Member of the North Vernon Limestone. Specimen found in Clark County, Indiana. Brachiopod existed in the Middle Devonian Period (Eifelian).
While this fossil is not complete, features I like are the muscle scars and exposed hinge teeth. It might be mixed in with other brachiopod fragments of Chonetes and Sprifier.
The Silver Creek Member ranges 0-9 meters in thickness through out Clark County. Described by (Campbell & Wickwire, 1955) as "homogeneous, fine-grained, bluish to drab or gray, argillaceous, magnesian limestone". I find it to be a light gray to whitish in color and quarried for cement. Maybe it is the reason Cementville exists with the Essroc plant in Clark County. It was named by C.E. Siebenthal in the 1901 Indiana Department of Geology and Natural Resources Annual Report 25.
Sources for identification:
Formations of Ordovician, Silurian, and Devonian Rocks in the vicinity of Hanover, Indiana Compiled by Guy Campbell and Grant T. Wickwire - January 1955.
Picture on fossilpictures.wordpress.com web site. Especially picture located lower left corner (click to enlarge).
Labels:
devonian,
indiana,
north vernon limestone,
silver creek member
Sunday, June 27, 2010
Jesse Earl Hyde Collection
Cladoselache Shark Fossil
Cleveland Shale - Upper Devonian Period
Geier Collections Center of Cincinnati Museum
Ohio - United States
The website describes itself this way, " This website contains images and descriptions of over one thousand glass lantern slides used by Prof. Jesse Earl Hyde (1884-1936), a professor who taught geology at Western Reserve University (now part of Case Western Reserve University) from 1915 until his death in 1936. The collection itself contains more than 2000 slides and hundreds of photographs made roughly from 1890 to the mid 1930's. These slides span a massive range of topics such the evolution of man, glaciers, Ohio geology, and the history of science just to name a few"
The images that interested me were of the Cladoselache shark: 675.7, 675.8, and 675.40. The last link has a picture that I hope will help me identify something I found in the New Albany Shale. Since I do not have permission to use the pictures from the Jesse Earl Hyde collection, I include in this post images I took while visiting the Cincinnati Museum Geier Collections Center.
Cladoselache Shark Pectoral Fins Fossil
Cleveland Shale - Upper Devonian Period
Geier Collections Center of Cincinnati Museum
Ohio - United States
Update (March 2020): Elizabeth Hyde Siman, Professor Jesse Hyde's granddaughter contacted me and this collection. I realized the university had moved the images from their geology server to the College of Arts and Sciences one. I have adjusted the links so they work again.
Saturday, June 26, 2010
Beargrass Creek Quarries
When looking at old fossil collections stored at museums and universities that contain specimens collected from the Louisville, Kentucky area, one sees localities like "Falls of the Ohio" or "Beargrass Creek". In previous posts, the Falls of the Ohio have been covered plus they have an excellent website.
The locality has somewhat faded into history. Beargrass Creek once hosted a number of quarries that I assume harvested Louisville limestone from the Silurian Period. As you can see from the pictures it has been a while since any rock was harvested from the Beargrass Creek area. An example of some fossils listed as having been found in the Beargrass Creek quarries: Cystihalysites nexus, Quepora huronensis, Syringopora hisingeri, Diorychopora tenuis, and Aulopora pygmaea. These species are just a few listed in Erwin Stumm's 1964 book that showed the specimens as being stored at Harvard University.
Today, one can see remnants of these quarries along the Beargrass Creek Greenway.
The actual Beargrass Creek visible from the path.
Rock walls becoming overgrown by vegetation.
Side note here are signs showing Louisville, Kentucky's sister cities: Mainz (Germany), Quito (Ecuador), Leeds (United Kingdom), La Plata (Argentina), Tamale (Ghana), Montpellier (France), Perm (Russia) and Jiujiang (China). It should be noted that Louisville is also twinned with Bushmills, Northern Ireland.
The locality has somewhat faded into history. Beargrass Creek once hosted a number of quarries that I assume harvested Louisville limestone from the Silurian Period. As you can see from the pictures it has been a while since any rock was harvested from the Beargrass Creek area. An example of some fossils listed as having been found in the Beargrass Creek quarries: Cystihalysites nexus, Quepora huronensis, Syringopora hisingeri, Diorychopora tenuis, and Aulopora pygmaea. These species are just a few listed in Erwin Stumm's 1964 book that showed the specimens as being stored at Harvard University.
Today, one can see remnants of these quarries along the Beargrass Creek Greenway.
The actual Beargrass Creek visible from the path.
Rock walls becoming overgrown by vegetation.
Side note here are signs showing Louisville, Kentucky's sister cities: Mainz (Germany), Quito (Ecuador), Leeds (United Kingdom), La Plata (Argentina), Tamale (Ghana), Montpellier (France), Perm (Russia) and Jiujiang (China). It should be noted that Louisville is also twinned with Bushmills, Northern Ireland.
Labels:
beargrass creek,
louisville kentucky,
silurian
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