Earthquakes. How do they occur? Nehal Murti. Earthquakes are very devastating as they destroy buildings and the lives of thousands of people. . Tectonic Earthquakes.By erling
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Overview of Convergent Plate Boundaries. ACTIVE. Olympic. Rainier. Crater Lake. Redwood. Lassen. ACTIVE. Lake Clark. Kenai Fjords. Katmai. ANCIENT. Yosemite. Kings Canyon. Sequoia. ANCIENT. Acadia. Shenandoah. Great Smoky. ANCIENT. Hot Springs. Big Bend. Convergence Types:.
Put your DRW on the box. 7-3b pg. 178 IN: What do you think happens when tectonic plates collide?. Convergent Plate Boundaries 10/7/14. These plates are moving around. Which means that they: Convergent Boundary Collide run into one another Divergent Boundary
Plates Move together : CONVERGENT PLATE BOUNDARIES. Learning goals : HOW ARE THE POSITIONS OF THE CONTINENTS CHANGED OVER TIME?. When plates collide or meet
WRITE WHAT IS IN GREEN. Type of Plate Boundaries. Divergent Plate Boundaries. Divergent Boundary: Between two lithospheric plates that are moving apart DI- vergent /DI-vide Rift Valleys: deep valleys at the center of a mid-ocean ridge
General Geology: Convergent plate boundaries Mass wasting . Instructor: Prof. Dr. Boris Natalin. Topics . Orogeny and orogenic belts Subduction zones Continental collisions Transform boundaries Hot spots. Mountain belts. Planes and mountains (cratons and orogens).
There are 3 types of Plate Boundaries. Each one has a type of STRESS on the rock & a way that it breaks, called a FAULT :. Divergent Boundaries Convergent Boundaries Transform Boundaries. Let’s break it down…. Divergent Boundaries. Place where 2 plates pull away from each other.
When the plates collide (or convergent plate boundaries). LO: to be able to explain what happens when plate boundaries meet. Key words we have learnt so far. Convergent Divergent Conservative Oceanic Constructive Crust Mantle Ocean ridge Plate Core Convection currents.
Plate Boundaries. colllisional. How collision builds mtns: processes are labeled on diagram. The topography of a mtn is build from a combination of physical (faulting and folding pushing the surface UP) and isostatic (the crust rises because it gets thicker and can float higher in
Plate Boundaries…. Divergent Boundaries (aka constructive boundaries). Rising convection currents force 2 plates apart Release of pressure on asthenosphere causes it to become molten and to rise Crust spreads New lithospheric material created.