The Isthmus of Panama.  20 million years ago the ocean covered the area where Panama is located today  Beneath the Earth's surface, two plates were.

Slides:



Advertisements
Similar presentations
Layers of the Earth.
Advertisements

So what has caused the continents to drift ??
The Earth.
Types of Plate Boundaries
Plate Tectonic Test Review Answers!
Landforms.
PLATE TECTONICS Why the Earth is Like It Is. What Did The Earth Look Like In The Past?
Mr. Burton 2.3 Notes Please Grab: 1. Your folder. 2. Writing Utensil. 3. Answer the following question: How does the surface of the earth move?
Edible Plate Tectonics. TECTONICS: From the Greek “tecton” – builder – architect The study of large features on Earth’s surface and the processes that.
EQ: What is the theory of plate tectonics?
Trench When two plates of oceanic crust collide, one plate sinks beneath the other. One of the plates is pushed beneath the deep-sea trench down toward.
Chapter 7 Earth’s Moving Crust
Types of Plate Boundaries
Created by Science Teachers Unit 4 Lesson ChangesTimeForcesAgents
1.3 Outline Plates Move Apart. I. Tectonic Plates Have Different Boundaries 1) Divergent boundary: occurs where plates move apart; mainly found in ocean.
How are these like the mantle?
Imagine the Earth as a hardboiled egg……………………. The thin brittle shell is the crust that humans live on. The thick jelly like white is the deep hot magma.
1.3 Notes Plates Move Apart.
Factors that Cause Tectonic Plate Movement
Forces Shaping the Earth
Volcanoes Earth and Space Science. How many are there? About 60 of the ~550 known active volcanoes erupt each year There are many more volcanoes underwater.
Tectonic Activity Plates. –Tectonic Plates –Convection Currents –Destructive Plate Boundaries –Constructive Plate Boundaries –Conservative Plate Boundaries.
Question Where are volcanoes found? What is a hot spot? Answer Volcanoes form along the boundaries of Earth's plates. An area where material from deep.
Plate Tectonics Evolution of the Earth.
Landforms.
Landforms What are the shapes the land takes and why? WG.4B Describe different landforms and the physical processes that cause their development [SUPPORTING.
Plate Boundaries. Destructive Plate Boundaries Also known as convergent boundaries or compressional boundaries. These cause violent volcanoes and earthquakes,
Awesome Links….copy and paste the URL’s
(Types of Plate Boundaries)
1F 9/5. 1F Isthmus Isthmus of Panama A narrow strip of land connecting two larger pieces of land.
Plates Move. Schedule Plate Movement Notes15-20 minutes ABCD Card Review10 Minutes Comic Strip Activity30-40 Minutes Exit ticket5-10 Minutes.
Internal Forces that Shape the Earth (Plate Actions)
Earth Science 9.3 Theory Tectonic Plates
Chapter 2: Plate Tectonics Theory of plate tectonics Proposed by Alfred Wegener Earth’s crust consists of plates that move or float on the mantle Movement.
These plates form, move, and subduct
Ch. 6 Plate Tectonics.
How Landforms Are Created
Types of Plate Boundaries.
The Problem with Continental Drift While Wegener was able to find evidence of continental drift, there were 2 major problems with his ideas: – Wegener.
Geology 12. Divergent Boundary /animations/basic_plate_boundari es.htm  Plates move apart.  The crust cracks and.
Essential Question: How does the constant movement of lithospheric plates cause major geological events on the earth’s surface? Standard: S6E5e. Recognize.
Continental Drift. Continental Drift Theory Most other scientists did not feel Wegener’s theory was true. That was because Wegener couldn’t come up with.
Divergent Boundaries (aka constructive boundaries) Rising convection currents force 2 plates apart Release of pressure on asthenosphere causes it to.
Plate Boundaries. Convergent Boundaries 2 plates move toward each other Destructive plate margins Old plate material is being recycled Oceanic crust.
Continental Drift Theory The hypothesis that Earth’s continents move on Earth’s surface. Wegner proposed this theory Sea Floor Spreading a process in which.
Types of Plate Boundaries After completing this section, students will identify that the Earth is made of geologic plates (Standard PI-041) and investigate.
PLATE TECTONICS Why the Earth is Like It Is What Did The Earth Look Like In The Past?
Landforms.
Volcanoes and Plate Tectonics A volcano is a weak spot in the crust where molten material, or magma, comes to the surface. Magma is a molten mixture of.
 Plate Tectonics refers to the movements of plates (large segments of continents and ocean) around the Earth’s surface.  These land masses are seen.
6.3 The Plates Move Apart Mrs. Avant. Boundary Types O Divergent: occurs where plates move apart. Most divergent boundaries are found in the ocean. O.
 Lithosphere is broken into huge plates and float on the asthenosphere. How Plates Move.
Warm up  Which landform is most likely to form where two oceanic plates push together?  A. folded mountains  B. mid-ocean ridge  C. river valley 
Plate Tectonics the movement of Earth.
Continental Drift and Plate Tectonics (notes pt. 2)
Plate Tectonics Evolution of the Earth.
Continental Drift Theory
CHAPTER 2 Plate Boundaries.
Geology Notes Part 6.
Continental Drift Theory
Plate Tectonics Evolution of the Earth.
9-3 Theory of Plate Tectonics
Physical Geography.
Plate Movements.
Oreo plate tectonics.
Landforms & Bodies of Water
Plate Tectonics, Physical Processes and Influence
9.3 Actions at Plate Boundaries
Plate Tectonics.
Plate Tectonics.
Presentation transcript:

The Isthmus of Panama

 20 million years ago the ocean covered the area where Panama is located today  Beneath the Earth's surface, two plates were slowly colliding into one another  This forced the Pacific Plate to slide slowly under the Caribbean Plate. The pressure and heat caused by this collision led to the formation of underwater volcanoes.

 More and more volcanic islands filled in the area over the next several million years.  Meanwhile, the movement of the two tectonic plates was also pushing up the sea floor, eventually forcing some areas above sea level.  Over time, massive amounts of sediment (sand, soil, and mud) were peeled away from North and South America by strong ocean currents and fed through the gaps between the newly forming islands—eventually this sediment filled in the gaps of the volcanic islands and the isthmus was formed

 Panama contains the Panama Canal which is extremely important to ‘maritime’ trade  Before the Panama Canal existed traders had to sail all the way down the coast of South America and around Cape Horn  The creation of the canal made trading easier and opened up countries located in that area of the world up to new trading partners

 Now that we see the importance that landform creation can have in your assigned groups please  1) tell me what makes your landform important/ special  2) did the creation of this landform serve any economic or political uses

 1) You will have the Isthmus of Suez  2) You will have the Straight of Gibraltar  3) You will have the Persian Gulf

REVIEW

 convergent boundary, also known as a destructive plate boundary (because of subduction—crust is destroyed)  In this boundary 2 or more plates move toward one another and can collide  During collisions between two continental plates, large mountain ranges, such as the Himalayas are formed.

 Divergent boundary (aka constructive boundary because as the plates move apart new crust is formed)  Plates move away from one another Divergent boundaries within continents initially produce rifts which produce rift valleys. Most active divergent plate boundaries occur between oceanic plates and exist as mid-oceanic ridges. Divergent boundaries also form volcanic islands which occur when the plates move apart to produce gaps which molten lava rises to fill.

 Transform fault—neither creates nor destroys the Earth’s crust  Transform faults show up on the seafloor as valleys that may be even deeper than the rift valleys of spreading ridges.

 An area of fairly level high ground  Plateaus can be formed by a number of processes:  1) upwelling of volcanic magma or spreading of lava  --Magma rises from the mantle causing the ground to swell upward, in this way large, flat areas of rock are uplifted. Plateaus can also be built up by lava spreading outward from cracks and weak areas in the crust.

 erosion by water and glaciers.  Plateaus can also be formed by the erosional processes of glaciers on mountain ranges, leaving them sitting between the mountain ranges. Water can also erode mountains and other landforms down into plateaus or they are pushed upwards by moving tectonic plates.

 A triangular tract of sediment (silt) deposited at the mouth of the river

 A narrow passage of water connecting two seas or two larger bodies of water.

 A piece of land almost surrounded by water or projecting out into a body of water.

 A sea or a stretch of water containing many island.

 A deep inlet of the sea almost surrounded by land, with a narrow mouth.

 A point or a head of land pointing into a body of water.

 1. What is an area of fairly level high ground called?  2. What is a sea or a stretch of water containing many island?  3. What is a point or a head of land pointing into a body of water called?  4. A deep inlet of the sea almost surrounded by land, with a narrow mouth is called what?  5. A narrow passage of water connecting two seas or two larger bodies of water is called what?  6. A piece of land almost surrounded by water or projecting out into a body of water is called what?  7. What is a triangular tract of sediment (silt) deposited at the mouth of the river called?  Terms  Archipelago  Plateau  Delta  Gulf  Straight  Peninsula  Cape