'Mountain belts' presentation slideshows

Crustal Deformation and Mountain Building

Crustal Deformation and Mountain Building. Behavior of rocks to stress & strain. Elastic Elastic limit Plastic Brittle. Stress. Strain. FOLDS. Anticline vs. syncline Hinge line (axis) Limb Axial plane Plunging fold Structural dome Structural basin. FOLDS. Interpreting folds

722 views • 53 slides

Classroom presentations to accompany Understanding Earth , 3rd edition

545 views • 46 slides

Ch 9 Notes

Ch 9 Notes. Mr. Russo Beaumont High School. Ch 9 Vocab Matrix (Pg 45). Divergent boundary Convergent boundary Transform fault boundary Oceanic Ridge Rift Valley Seafloor Spreading Subduction Zone Trench Continental Volcanic Arc Volcanic Island Arc Paleomagnetism Hot Spot.

727 views • 38 slides

GLY 326 Structural Geology

GLY 326 Structural Geology. Lecture 7 The anatomy of continents. Autumn , 2015. The Wilson Cycle. The Wilson Cycle. The Wilson Cycle. The Wilson Cycle. The Wilson Cycle. The Wilson Cycle. The Wilson Cycle. Structures of Continents. continents are made and deformed by plate motion

389 views • 38 slides

tom.h.wilson tom.wilson@geo.wvu

Geology 351 - Geomath. Equation Manipulation illustrated around the concept of Isostacy. Segment II. tom.h.wilson tom.wilson@geo.wvu.edu. Department of Geology and Geography West Virginia University Morgantown, WV. Chapter 3: Equations and how to manipulate them

375 views • 37 slides

tom.h.wilson tom.wilson@geo.wvu

Geology 351 - Geomath. Equation Manipulation illustrated around the concept of Isostacy. Segment II. tom.h.wilson tom.wilson@geo.wvu.edu. Department of Geology and Geography West Virginia University Morgantown, WV. Don't forget. Hand in problem 2.13 & 2.15 today

375 views • 37 slides

Geol 351 - Geomath

Geol 351 - Geomath. Isostacy II - Wrap up isostacy and begin working on the settling velocity lab. tom.h.wilson tom. wilson@mail.wvu.edu. Department of Geology and Geography West Virginia University Morgantown, WV. Explanations for lowered gravity over mountain belts.

362 views • 25 slides

Continental Crust and Mountain Belts

Continental Crust and Mountain Belts. Continents are composed of two basic types of terrain Cratons , where there hasn't been significant structural deformation lately

499 views • 14 slides

Our Changing Earth

Our Changing Earth. Mr Greathouse Ch 3.1. Movement of Rocks Builds Mountains. Mountains An area of land that rises steeply compared to the area around it (Everest, Lemmon) Mountain Range Long lines of mountains formed at the same time and by the same process

366 views • 13 slides

Lecture Outlines Physical Geology, 10/e

309 views • 11 slides