Slide 1 Keys to Sedimentary Environments I Sediment Composition and Texture II Sedimentary Structures - Inorganic - Organic (Trace Fossils) III Geometry of Rock Body &…
Slide 1 But why clay- It is important to know where we are coming from, since the course of study in MNA/IMACS centers on clay and clay minerals basically Slide 2 How are…
Slide 1 What do we use the fossil record for? 3. Interpreting past environments http://www.wsgs.uwyo.edu/Coal/coal_brochure/images/fig1_swamp.jpg http://oceanworld.tamu.edu/students/coral/images/coral_reef_1.jpg…
Slide 1 Slide 2 Slide 3 BACKGROUND MATERIAL AND FACTUAL CHRONOLOGY Field study of rocks involves measuring the thicknesses of different rock units, called formations, and…
Slide 1 By: Julie Hedegaard Slide 2 The story Albert dates back to the early 1950's when local cattle shippers were feeding great numbers of cattle to the prime grade…
Recrystallization of limestone to dolomite Presented by: Zohreh Baghban Professor: Dr. Shafiee 10/30/2014 Content Recrystallization vs. dolomitization Carbonate rocks Limestone…
Sedimentary Rocks All places on Earth are, at any moment, either EROSIONAL or DEPOSITIONAL High places are erosional Low places are depositional Sedimentary Rocks Are made…
Rocks Rocks Sedimentary, Igneous, and Metamorphic 2 There are 3 basic types of rocks â sedimentary, igneous and metamorphic. Rocks are made of one or more kinds of minerals…