'Sediment layers' presentation slideshows

Sedimentary Rocks

662 views • 45 slides

Algorithms Overview

Algorithms Overview. Hernan G. Arango Institute of Marine and Coastal Sciences Rutgers University. 2004 ROMS/TOMS European Workshop CNR-ISMAR, Venice, October 18-20. Outline. ROMS/TOMS algorithms status ROMS/TOMS future releases How does one build an adjoint model? Ensemble prediction

513 views • 34 slides

Extension of the Variable Rotated Parabolic Equation to Problems Involving Variable Topography

Extension of the Variable Rotated Parabolic Equation to Problems Involving Variable Topography. Jon M. Collis and William L. Siegmann Rensselaer Polytechnic Institute Troy, New York Michael D. Collins Naval Research Laboratory Washington, D.C.

165 views • 16 slides

Relative Dating

448 views • 15 slides

The Phosphorous Cycle

The Phosphorous Cycle. Section 4.5. The Phosphorous Cycle. Uses of phosphorous by organisms: Phosphorous, like nitrogen and carbon, is an important element needed by organisms. The Phosphorous Cycle. Cell membranes: They are made of a phospholipid bilayer in all cells.

269 views • 13 slides

Story In The Rocks!

Story In The Rocks!. Andrew Fiora and Sarah Draper. Weathering. Weathering involves 2 processes, chemical and physical. Chemical Weathering involves chemical change in some of minerals within rock.

207 views • 13 slides

EVIDENCE OF EVOLUTION

EVIDENCE OF EVOLUTION. EVOLUTION & THE FOSSIL RECORD. INTRODUCTION. Evolution: change in a species over time Organic Evolution: changes in living things Data from organic evolution explains two things: Differences in structure, function, and and behavior among living things

350 views • 11 slides

Sedimentary Rock

Sedimentary Rock. By : Akosua , Quentin , Salimah , And the Awesome Toni J. What is SedimentaryRock ?. Sedimentary rock is formed at or near the Earth's surface by the settling and accumulation of rocks, minerals, or the remains of plants and animals. Clastic sedimentary rock.

305 views • 10 slides

Fossils

704 views • 10 slides

Sedimentary Structures

Sedimentary Structures. Clues to depositional environments. Bedding - layering!. Layering of sediments is common due to episodic deposition In most cases the layers are close to horizontal at the time of deposition Layering may survive lithification. Loose sediment - Merrimack Valley.

984 views • 8 slides