Teaching Notes and Tips

Teaching Notes and Tips

TEACHING NOTES AND TIPS. The RCL sedimentary module is planned as a 3-part sequence. (1) The very short powerpoint Rupturing Continental Lithosphere: Introduction (from Dorsey 2013) is the starting point*. It will give students a preview of the scientific.

Quantitative Textural and Microstructural Study of Orthogneiss Deformed at Increasing

Quantitative Textural and Microstructural Study of Orthogneiss Deformed at Increasing

Quantitative textural and microstructural study of orthogneiss deformed at increasing metamorphic grade: contributioon of solid state annealing to metamorphic textures. Pavla Stipska, Ondrej Lexa Karel Schulamann.

1. Detailed Sample Description and Background

1. Detailed Sample Description and Background

1. Detailed sample description and background. The majority of the xenoliths in this study can be classified into one of two groups, commonly referred to as Groups I and II (Frey and Prinz, 1978). Menzies (1983) refined the classification but referred.

Instructor S Notes for Stratigraphy Cogsketch Geoscience Worksheet

Instructor S Notes for Stratigraphy Cogsketch Geoscience Worksheet

Instructor s Notes for Stratigraphy CogSketch geoscience worksheet. This worksheet uses the sketch-understanding program with built-in tutor: CogSketch. Therefore, students, instructors, and/or institution computer labs need to download the program from.

Columbian Exchange Projectname

Columbian Exchange Projectname

Columbian Exchange ProjectName. Guided Reading. 1. How many miles separate America and Europe? 2. How many years passed between the break up of Pangaea and the time humans (Homo Sapiens) arrived in the Americas?

Blue Mountain Plateaus

Blue Mountain Plateaus

Blue Mountain Plateaus. Plateaus in the Pacific Northwest are predominantly underlain by stacked flows of the Columbia River Basalts and form extensive elevated plains bounded on one or more sides by steep slopes hundreds of feet above adjoining areas.

From: Slava Solomatov Slava Dao

From: Slava Solomatov Slava Dao

Measurements of Velocities and Elastic Properties at High Pressures and Temperatures. The best-resolved properties of Earth s interior are the sound velocities Vp and Vs, and the density. Beyond average radial properties, seismological studies now reveal.

Source: Panorama of Landforms, NASA

Source: Panorama of Landforms, NASA

Source: Panorama of Landforms, NASA. In this lesson, you will also study the factors that change these landforms called physical processes. Some landforms are created by the action of wind, water, and ice. These physical processes change the Earth's surface.

Chapter 2 Earth Systems: Processes and Interactions

Chapter 2 Earth Systems: Processes and Interactions

Chapter 2 Earth Systems: Processes and Interactions. 2.1 The Solid Earth System: Components and Processes. Earth s interior consists of crust, mantle and core; the crust and the uppermost. mantle together constitute the lithosphere.

At This Point You Should Have a Good Understanding of the Rock Cycle, the 3 Main Classifications

At This Point You Should Have a Good Understanding of the Rock Cycle, the 3 Main Classifications

At this point you should have a good understanding of the rock cycle, the 3 main classifications of rocks (sedimentary, metamorphic, and igneous) and the forces/processes that change them. You should also have a basic understanding of the characteristics.

Geomorphic Assessmentof the Middle and Lower Swan Lake Watershed, Calhoun Division Of

Geomorphic Assessmentof the Middle and Lower Swan Lake Watershed, Calhoun Division Of

Geomorphic Assessmentof the Middle and Lower Swan Lake Watershed, Calhoun Division of Two Rivers National Wildlife Refuge. Laura Keefer, M.S. Fluvial Geomorphologist. Watershed Specialist. Illinois State Water Survey. Institute of Natural Resource Sustainability.

Casier, J.-G. and Olempska, E. (In Print). Middle Frasnian (Devonian) Ostracods from The

Casier, J.-G. and Olempska, E. (In Print). Middle Frasnian (Devonian) Ostracods from The

Casier, J.-G. and Olempska, E. (in print). Middle Frasnian (Devonian) ostracods from the Frasnes railway section (Dinant Synclinorium, Belgium).- Bulletin de l Institut royal des Sciences naturelles de Belgique, Sciences de la Terre 78.

Earth Sciencestudy Guide Plate Tectonics & Earthquakes

Earth Sciencestudy Guide Plate Tectonics & Earthquakes

Earth ScienceStudy Guide Plate Tectonics & Earthquakes. The Theory of Continental Drift. Francis Bacon (1620) proposed that the continents once fit together. Alfred Wegener (1912), a German meteorologist, came up with The Theory of Continental Drift which stated that.

III.Course Textbooks, Manuals, Or Other Required Materials

III.Course Textbooks, Manuals, Or Other Required Materials

I.Course Description. Introduction to Geology I (physical geology) is a study of geologic processes and features with emphasis on plate tectonics. Topics include the origin of magma, volcanoes, earthquakes, weathering, sediments, metamorphism, rivers.

Pleading for a New DCB in the Historical German Deep Facies of Sauerland Near Stockum

Pleading for a New DCB in the Historical German Deep Facies of Sauerland Near Stockum

Pleading for a new DCB in the historical German deep facies of Sauerland near Stockum. Maurice Streel, Geology Department, University of Liège, Belgium Dieter Korn, Museum fürNaturkunde, Invalidenstr. 43, 10115 Berlin, Germany.

Western Basin & Range Workshop White Paper, Jan. 14-15, 2008, Univ. of Nevada, Reno

Western Basin & Range Workshop White Paper, Jan. 14-15, 2008, Univ. of Nevada, Reno

Nevada Great Basin Community Velocity Model Workshop. January 14-15, 2008 at the University of Nevada, Reno. Draft Summary by J. Louie, 7/23/08. The Nevada Seismological Lab convened a 2-day workshop on creating a Nevada Great Basin Community Velocity.