A Combinatoric Approach to the Study of Mineral- Molecule Interactions A Combinatoric Approach to the Study of Mineral- Molecule Interactions Frontiers.
Source of course material Dr. Olaf Medenbach, Ruhr-Universität Bochum Optical microscopy of rock-forming minerals, G. Wörner, USTC Hefei Compact Course.
Monday November 02, 2009 Open your notebooks. Write down today’s questions. Today’s Theme: What is a mineral? –What are the ways that minerals can.
The Rock Cycle Indicates agents of change and the types of rock that are present on Earth and under what conditions they change.
Classification based upon formation. Igneous rocks form from molten lava. What’s the difference between magma and lava? The formation of igneous rocks.
Matching Metamorphi c Rocks with their Sedimentar y Source Rocks.
Ch 9. Weathering A. Mechanical Weathering B. Chemical Weathering C. Soil.
What is the volume of each cube? 1. A.What is the density of each sample? A.Would each sample float or sink in pure water? 2.
Color is useful in recognizing some minerals, but not all N. Lindsley-Griffin, 1998.
Earth Science Standards 3.a - Students know features of the ocean floor (magnetic patterns, age, and sea-floor topography) provide evidence of plate tectonics.
Weathering and Erosion. Weathering Alteration of rock materials during exposure to air, moisture, and organic matter. Responsible for limited changes.
Minerals of the Earth’s Crust Fluorescence is the ability that some minerals have to glow under ultraviolet light. The beauty of mineral fluorescence is.