Ammonoidea of the Lower Cretaceous deposits (Late Berriasian, Valanginian.Early Hauterivian) from Štramberk, Czech Republic.1 Institute of Geology, Academy of Sciences of the Czech Republic, Rozvojová 135.165 02 Praha 6, Czech Republic;
Center # 6: Interactives: Rock Cycle.Get a computer and login.To get to the website, do a Google search for Interactives Rock Cycle, go to my blog for a direct link, or type in.Part I Introduction.1. Label the blanks in the diagram below after looking at the Introduction page
Geology 115/History 150 Name(s).Lab 6: Minerals and metamorphic rocks.A mineral is a naturally-occurring, solid, usually inorganic element or compound with a definite crystal structure and chemical composition which varies only within specific limits. Rocks are merely aggregates of minerals
Semester 1 Exam Study Guide Key.Scientific Method.1. Steps of the scientific method.State the question, collect info, form hypothesis, test, record data, draw conclusion.2. Variables: identify controls, independent and dependent
Designing Sedimentary Geology Courses Around Field Projects With Realistic Scenarios.Bosiljka Glumac.Department of Geology.Smith College.The Smith College Sedimentology course is an example of a course structured around projects, most of which are field
Virtual Earthquake Lab.Objective: The student will learn about the causes of earthquakes, the types of seismic waves and how scientists use seismographic information to determine thelocation and strength of an earthquake.Materials: Internet access and lab sheet.Procedure and Questions
PHYSICAL GEOGRAPHY 1 - LANEY COLLEGE - SPRING 2016.Instructor: Mark J. Rauzon;.Office Hours in A275 Mon./Wed. 12:30-1:00; Tues./Thur. 12:15-1:15.Course Description.This is a general course that introduces the basis elements of the earth s physical systems
Geological Report Guidelines for New Development on Oceanfront Properties.Produced by the Coastal Processes and Hazards Working Group and Oregon Coastal Management Program staff (including DLCD, DOGAMI, and OPRD), this is a list of geologic factors, analyses
CAVE and KARST AREA BOILERPLATE.AFFECTED ENVIRONMENT #1: Gypsum Karst.The project is located in gypsum karst terrain, which may contain sinkholes, sinking streams, caves, and springs. These features, as well as occasional fissures and discontinuities
SCI 675 Oregon Field Geology: West Coast to Cascades.Pretrip meeting Wednesday Aug. 6th 5:00 7:00 Rogers Hall rm. 218.Course is taught in the field. Aug 9th to 15th meet at South Campus parking lot
You will need: Topic Y3 Science Strand Rocks.We will provide.The links to the websites and the contents of the web pages associated with such links specified on this list (hereafter collectively referred to as the Links ) have been checked by Hamilton
High School Geology.Carlsbad Caverns National Park.High School Geology Curriculum.A. The present is the key to the past: unlocking the geologic history of southeastern New Mexico and west Texas 4.B. Putting the puzzle together; internal structure of the Earth and Pangean geography 8
Course Syllabus.Natural Disasters and Environmental Geology (GEOL 104).College of Southern Idaho (CSI) Spring 2015.Instructor: Travis Phillips.Office Hours: M-F 7:30-4:00.Class Day/Time: M-F 5th Period.Required Course Materials
PLATE TECTONICS.Use the maps provided to answers the following questions. The map title is above the questions.Some maps are used on both sides.LIVING ON THE EDGE.Which two minor plates are colliding with Oregon and Washington?.When was the San Francisco earthquake?
2012 Fall Semester PreAP World Geography Final Exam Review.Unit 1: Introduction, Map Skills, and Landforms.What is the difference between absolute and relative location?.What is the difference between formal and functional regions? Identify examples of each
Geology 10 - Physical Geology.Instructor: Dr. Tim Horner.Office: Placer Hall rm. 1018.Office Hours: Monday, Tuesday, Thursday 11:00 12:00 or by appointment.General Information.The objective of this course is to provide an understanding of earth materials