How to use this template (DELETE THIS SLIDE) This is only a guide, you may add to this if you wish. Do not add pictures as background, to hard to see and.

Slides:



Advertisements
Similar presentations
By Ryan Arthur and Kole Patton
Advertisements

Relative Age Dating and Superposition
Highlight & place your title here Highlight & write in your name here Holy Sepulcher Catholic School Grade ? Use the Student Guide to the HSS PJAS Presentation.
Modeling Geologic Columns With Sand Art By Debra Rockey Wellsburg Middle School 1.Prepare the plastic tube. One end should be permanently sealed. If necessary,
Geologic Mapping of an Area Near Crook Creek, SD Purpose: To collect data necessary for the construction of a geologic map and cross-section of.
Middle Ordovician to Late Silurian Geology Eastern United States.
Stratigraphy and fossils
Ordovician Utica Shale Utica Shale deposited during Ordovician Taconic Orogeny.
_____/5 “logistics” Title, scale (bar and ratio), author, date, N arrow, explanation (rock units (oldest at the bottom) with symbols and ages, strike and.
Hydrothermal Dolomites in Central Kentucky:
The Carbon Isotope Record of the Great Ordovician Biodiversification Event Carlos Y. Vélez.
Earth History- Table of Contents RELATIVE vs. ABSOLUTE LAWS UNCONFORMITIES GEOLOGIC SECTIONS.
Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?
Principles of Relative Dating
Looking at Trenton–Black River Reservoirs: Outcrops Analogs in Kentucky Dave Harris Kentucky Geological Survey University of Kentucky.
High Resolution Stratigraphy and Parasequences of the Oriskany Sandstone, Mapleton, Pennsylvania Jason Abplanalp and David Lehmann, Juniata College, Huntingdon,
How do scientists construct the geologic history of an area?
Sharing what we do ~ Wrestling with Time using 50 minute group activities for hundreds of students. Dep’t Earth and Ocean Sciences Stuart Sutherland:
Terms for Geologic Time
Geology 350/Biology 350 INVERTEBRATE PALEONTOLOGY FIELD PROJECT: FOSSIL COLLECTING, IDENTIFICATION, AND REPORT WRITING Stephen A. Leslie, Department of.
Earth Science Topic #13 Review Game
Regional Geology of Khwisero District, Kenya April 2012 Scott Patterson.
Student Name Teacher Name Section Number
Porosity, Carbonate Content and TOC
A Geological Overview of North Central West Virginia: Observations from the Field Lyndsey Lieb and Angela Lands, Kennesaw State University and Mike Kelly.
Determining geological ages
Earth History- Table of Contents RELATIVE vs. ABSOLUTE LAWS UNCONFORMITIES GEOLOGIC SECTIONS.
Ch.6 Earth’s History. Who’s got the TIME? RELATIVE: order/sequence known, but not the actual date of occurrence. “Time Line” ABSOLUTE: actual date determined.
News and information Partner list posted Gas up vans before tomorrow morning Leave some space in your notebook NIU students with yellow GPS come see me.
Pacific NW Geology. Course Goals 1.Analyze geologic features for rock type and depositional history and interpret the geologic history 2.Develop place-based.
LITHOSTRATIGRAPHY Upper Ordovician Strata of the Appalachian Basin Utica Shale Play Book Study - Canonsburg, PA - July 14, 2015 John Hickman, Cortland.
Dr. Tark Hamilton Camosun College
How to Write A Lab Report
Directions: Map 1: On the first map, determine the contour interval. Create the cross-section or profile from point A to point A’ Map 2: On the second.
The Stratigraphic Record
Sedimentary Geology Geos 240 – Chapter 3-3 Sedimentary Petrology-3 Dr. Tark Hamilton Camosun College.
Are the Recently Redefined Dayton Formation (Silurian, Llandovery, Telychian) and Dayton Limestone of Orton, the Celebrated Building Stone of Ohio, the.
Stratigraphy Stratigraphy is the branch of geology that deals with the arrangement of rocks in layers.
EARTH HISTORY UNIT MS. MITCHELL 9 TH GRADE EARTH SCIENCE VICTORIA MITCHELL 1.
Student Name Student ID Number Date of Presentation Midpoint Review [School] Title of Project.
Student Name Student ID Number Date of Presentation Midpoint Review [School] Title of Project.
How to Match (Correlate) Rock Columns These 3 columns represent rock layers from 3 separate areas. Some columns may be missing layers due to erosion. No.
Before the 1700’s, scientists thought that the Earth was only 6,000 years old. This mindset was based on biblical references.
Interpreting Ancient Environments
A Geological Overview of North Central West Virginia: Observations from the Field Lyndsey Lieb and Angela Lands, KSU and Mike Kelly and Minjuan Cheng of.
Models of the Earth Section 3 Section 3: Types of Maps Preview Key Ideas Topographic Maps Topographic Maps and Contour Lines Index Contour, Contour Interval,
EBS101 ENGINEERING GEOLOGY DR HAREYANI ZABIDI
Earth’s History Introduction: The earth is about 4.6 billion years old. Much of its history is recorded in the rock. Observations of fossils, rock types,
Research Proposal Presentation Template KHS 220 – Research Methods.
Geology 1023 Cordillera and Appalachians. Orogenic (mobile) belts At the edges of continents Platform sequence that gets buckled by collision Also volcanism,
Aim: How can we describe major events in Earth’s history? Do Now: How did Early Earth’s atmosphere differ from modern Earth? Could early Earth support.
Geologic Sequencing: The order of geologic events
Earth History- Table of Contents
Appalachian storage Hub (ASH) project
Relative Age Quiz.
Section 21.1 Study Guide Section 21.1 Main Ideas
Unit 2: Relative Dating - Part 2
Geologic Time Geologic Time Notes.
Department of Geology, University of Dhaka Maps and Map Reading Lab.
SACRAMENTO STATE Geology 103A Sedimentology and Stratigraphy Tim Horner Geology Department, CSU Sacramento Lecture #16: Stratigraphy Reading assignments:
Harry Williams, Historical Geology
7th grade Science Date My Name - 7th grade
Northern Iraq By Dr.Muhamed F. Omer
Geologic Time Geologic Time Notes.
Paleoecology Lab: 2 Versions
SACRAMENTO STATE Geology 103A Sedimentology and Stratigraphy Tim Horner Geology Department, CSU Sacramento Lecture #19: Carbonate components and classification.
Title Cover Page You can add slides to print your title in larger text if needed but remove after. This page is for teacher and should not be on the board!
Timing the Geologic Record
Understanding Earth Fourth Edition Chapter 10: The Rock Record and the
Presentation transcript:

How to use this template (DELETE THIS SLIDE) This is only a guide, you may add to this if you wish. Do not add pictures as background, to hard to see and looks messy. Less is more, don’t fill slides with words, add brief bullets and a picture or diagram. You should explain in your talk not have other read your slide. Your presentation needs to be 5 minutes long so practice and be sure to hit all important points and discussions. Be sure to cite everything that is not yours!!!

Ordovician Carbonates in Northwest Lewis and Parts of Southeast Jefferson Counties Andrews, J Teacher Block 1

Purpose Statement Using field data collected personally and with other geologists from 2003 field season. “Rework” the complicated naming system that is defined previously.

Introduction Collecting field data (via walking waterways) Naming system used incorrectly. Rocks in this area were formed underway and have fossils in the rocks. Titus 1986 and Isachsen 2000 Harvard Geology department

Methods All researchers including myself walked rock outcrops where ever possible. Measurements of the formations made with Jacobs Staff All data recorded, faults, dipping layers and fauna

Results Rock layers were described by Johnsen (1971) and Walker (1973) based mainly on formation thickness and fauna. Discuss results of methods of research Any possible issues with the research?

Discussion Formational ID new What are your conclusions from your research? What are the results of this research? Compare results to you purpose statement

Age Formation Lithology & Contact Description Average Thickness (m) Fuana System Series Group Middle Ordovician Mohawkian Trenton Hillier (Cobourg) Base: See top of Stueben Ls, mostly Micritic. Top: Erosional surface capped by phosphatic rich beds. 8 Hormotoma, Fusispira, Conularia trentonensi, Rafinesquina deltoidea Steuben (Cobourg) Base: base of criniodal grainstone that has no Shale interbeds Top: Sparry grainstone grading to micritic packstone. Contact can span over 1m. 8 Rafinesquina deltoidea, Triarthrus eatoni, Climacograptus Denley (Denmark) Base: Shale beds increase to 5-8cm. Ls increase and are micritic Top: Shale interbeds disappear, top is defined by last shale interbed uncertian Cryptolithus, Paraspora, Trocholites, Rafinesquina, Hormotoma, Resserela Sugar River (Shoreham) Base: Ls beds decrease to (5-8cm) and are sparry. Contact sharp to gradational Top:Defined by Base of Denley Trocholites, Cryptolithus, Prasopora Kings Falls (Kirkfield) Base: lowest in series of 12-25cm thick beds contianing para-ripples Top: Bed thickness decreases but still variable Triplesia, Sowerbyella, Cryptolithus pora orientalis, Rafinesquina, Parastrophina Napanee (Rockland) Base: thin to thick, grey to brown calcilutites interbedded with shale, Basel beds are often graded (disconformity) Top: Beds become more sparry and fosiliferous Doleroides ottawanus, Triplesia cuspidata, Paucicrura- Dalmanella rogata, Sowerbyella Triarthrus Cryptolithus Trilobites Prasopora Sowerbyella

Age Formation Lithology & Contact Description Average Thickness (m) Fuana System Series Group Middle Ordovician Mohawkian Black River Watertown (Chaumont) Base:Base of thick to massive weathering Ls beds. Top: Top of a set of thck to massive weathering Ls containing Chert nodules 6 (chephalopods) Actinoceras tenuifilum, Endoceras, Gojioceras, Tetradium fibratum Lowville Base: Top of Pamelia Top: Dark grey micritic Ls containing Gastropods 8-18 Phytopsis tubulosa, Hormotoma sp. Pamelia Base: arkosic conglomerate or Ss or Dolostone. (nonconformity) Top: where a 3.0m interval has a dolostone/Ls ratio of 1:1, also placed at top of last dolostone bed Tetradium syringoporoides, PreCambrianGniess?? Brachiopods

Conclusion Work done by Kay (1930’s) was correct and properly cited, thus must be used (ACSN 1982). Future research included mapping of faults for natural gas and the use of radiometric dating.

References American Commission on stratigraphic Nomenclature, 1982, note1 –Organization and objectives of the Stratigraphic Commission: American Association of Petroleum Geologists Bulletin, v. 31, no. 3, p Chenoweth, A. P Statistical methods Applied to Trentonian Stratigraphy in New York. Bulletin of the Geological Society of America. Volume 63, pp Cushing, H. P Lower portion of the Paleozoic sections in northwestern New York. Geological Society of America. Bulletin 19: Fisher, D. W Correlation of the Ordovician rocks of New York State. New York State museum and science service. Map and chart series 3. Folk, R.L., 1962, Spectral subdivisions of limestone types, in W.E. Ham (ed.), classification of carbonate rocks: American Association of Petroleum Geologists Mem. 1 p Isachsen, W. Y., Landing, E., Lauber, M. J., Rickard, V. L., Rogers, B. W Geology of New York, A simplified account. Second edition. New York State Museum. Johnsen, H. J The Limestones of Jefferson County, New York. N.Y. State Museum and science service. Map and chart series 13. Kay, G. M The Ordovician Trenton Group in Northwestern New York: Stratigraphy of the lower and upper limestone formations. American Journal of Science. Kay, G. M Stratigraphy of the Trenton group. Geological Society of America. Bulletin 48 pp Titus, R. Fossil Communities of the Upper Trenton Group (Ordovician) of New York State. Journal of Paleontology. Volume 60, no. 4, pp Walker, K.R Stratigraphy and Environmental Sedimentology of Middle Ordovician Black River Group in the Type Area- New York State. N.Y. State Museum and science service. Bulletin 419. Winder, C. G Paleoecological interpretation of Middle Ordovician statigraphy in southern Onartio, Canada. Ordovician and Silurian stratigraphy and correlations. Inter. Geol. Cong., Copenhagen, Denmark 21: