Processes and Land forms along the Convergent Plate Boundary (1).pptx

RyeAguirre 290 views 18 slides Feb 15, 2023
Slide 1
Slide 1 of 18
Slide 1
1
Slide 2
2
Slide 3
3
Slide 4
4
Slide 5
5
Slide 6
6
Slide 7
7
Slide 8
8
Slide 9
9
Slide 10
10
Slide 11
11
Slide 12
12
Slide 13
13
Slide 14
14
Slide 15
15
Slide 16
16
Slide 17
17
Slide 18
18

About This Presentation

Earth Science


Slide Content

PROCESSES AND LAND FORMS ALONG THE CONVERGENT P L AT E B O U N DARY With Sir Rye

Explain the different processes that occur along the plate boundaries (S10ES –Iaj-36.3) Objectives

Make sure you have the following before we start: Have you completed your requirements from your previous teacher? The worksheets for this week's activities

Kamusta?

Convergent Divergent Transform Shear Compression Tension

Convergent Plate Boundary Plates move towards each other Either one plate go below or two plates will crumple as they collide Forms mountains, volcanoes, trenches, and earthquakes “Collide” Compressional Stress Denser Plate always go down Less Dense Plate go up

Types of Convergent Plate Boundaries Depending on the type of plates that are colliding Oceanic - Continental Convergent Plate Boundary Oceanic - Oceanic Convergent Plate Boundary Continental - Continental Convergent Plate Boundary

Denser Plate always go down Less Dense Plate go up Oceanic plate=denser=go down Called Subduction, this creates Trenches Remember Subducted Plate become Magma Continental plate=less dense=go up Creates Volcanic arcs Earthquakes Oceanic - Continental Convergent Plate Boundary

Examples

Examples

Denser Plate always go down Less Dense Plate go up Old Oceanic plate=denser=go down Called Subduction, this creates Deeper Trenches Remember Subducted Plate become Magma Young plate=less dense=go up Creates Island arcs or Volcanic Island arcs Earthquakes Oceanic - Oceanic Convergent Plate Boundary

Examples

Examples

Examples North American Plate and Pacific Plate Forms Aleutian Volcanic Island Arc

Denser Plate always go down Less Dense Plate go up Two Continental Collide push each other upwards Same density = No subduction = No Magma = No volcanoes formed Mountains or Mountain Ranges Earthquakes Continental - Continental Convergent Plate Boundary

Examples Indian Plate and Eurasian plate Himalayas Mountain Range

TRENCHES ISLAND ARC MOUNTAIN RANGES VOLCANIC ARC EARTHQUAKE

Thank you for attending!
Tags