GG103 Nasir Gadzar.

Slides:



Advertisements
Similar presentations
The Parts of a Volcano.
Advertisements

Mountain Building Folding Faulting Volcanoes.
Introduction Volcano, mountain or hill formed by the accumulation of materials erupted through one or more openings (called volcanic vents) in the earth's.
Volcanoes Animation of a volcano.
Chapter 7 Lesson 3 Volcanoes
Essential Questions How do plate tectonics influence the formation of volcanoes? Where are the major zones of volcanism? What are the parts of a volcano?
Photograph by R. McGimsey on 15 July 1990 Mount Mageik volcano viewed from the Valley of Ten Thousand Smokes, Katmai National Park and Preserve, Alaska.
What are the three types of volcanoes and what type of eruptions does each volcano have?
Different Types of Volcanoes
1.Crater– bowl-shaped formation at the top of a volcano.
Three different types of volcanoes exist; Volcano An opening in Earth’s crust through which igneous matter (lava, ash, cinder, and gases) are erupted.
Volcanic Landforms Key Idea: The shape of a volcanic landform is determined by the materials produced during an eruption.
Volcanic Landforms 6 th Grade. 2 Kinds of Volcanic Eruptions Quiet Eruptions: – If magma is low in silica – Lava is low in viscosity and flows easily.
3 TYPES OF VOLCANOES. SHEILD HOW DO THEY FORM? Thin layers of lava pour out a vent and harden on top of previous layers.
Introduction Video Clip
Volcanoes : Volcanic Landforms.
VOLCANOES. What is a Volcano? A volcano is a weak spot in the crust where Magma, comes to the surface. Volcanic activity is a constructive force that.
Volcanoes.
V o l c a n o e s Cascades Volcanoes The Distribution of volcanoes.
Mountain Building Folding Faulting Most Major Mountain ranges were formed by the collision of continental Plates.
Volcanoes Chapter 9 Sections 1,2 and 3 VOLCANOES.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,
A volcano is a place (usually a mountain) where magma reaches Earth’s surface.
Volcanoes Openings in the Earths Crust That Lets Magma Through and Often Forms a Mountain.
VOLCANOES How they work. WHAT IS A VOLCANO? A mountain or hill having a crater or vent through which lava, rock fragments, hot vapor, and gas are being.
How do volcanoes form and what affect do they have on the Earth?
Volcanic Landforms 6 th Grade. 2 Kinds of Volcanic Eruptions Quiet Eruptions: – If magma is low in silica – Lava is low in viscosity and flows easily.
Mountain Building Folding Faulting Volcanoes.
Volcanoes Chapter 9 Sections 1,2 and 3 VOLCANOES.
Volcanoes How they are made? A Volcano is a mountain that opens downward to a a pool of molten rock below the surface of the earth. The extreme presser.
Types of Volcanoes.
Volcanoes 6.2.
Students will be able to explain why a volcano erupts and describe how volcanoes build land. Chapter 4 Lesson 2 Volcanoes.
Volcanoes. A Volcano is… A geographic feature on the Earth’s surface (as well as other planets) where magma erupts through the Earth’s surface. Volcanoes.
Lets Review……. Magma Chamber Lies inside the earth. Stores hot, melted rock called magma.
Volcanoes and Earth’s Moving Parts
Volcano Presentation Courtney Boyce, Justin Watkins and Bridget Egan.
Copyright 2009 abcteach.com Volcanoes. copyright 2009 abcteach.com Volcano Diagram.
A volcano is an opening, or vent, in the Earth’s crust through which magma and gases are expelled.
Volcanoes By: Amy Axelrood.
Pangea: The hypothetical landmass that existed when all continents were joined, from about 300 to 200 million years ago.
 Folding  Faulting  Volcanoes  Most major mountain ranges were formed by the collision of continental plates.
volcanism:any activity that includes the movement of magma toward the surface of the Earth volcano: place where magma reaches the surface What are volcanoes?
Introduction to Volcanoes Scripps Classroom Connection.
Volcanoes Chapter 9 Sections 1, 2,and 3 Pages Write down the underlined items.
Pangea: The hypothetical landmass that existed when all continents were joined, from about 300 to 200 million years ago.
1.3: T YPES OF V OLCANOES 1. Describe basic shapes of volcanoes. 2. Compare the features of volcanoes. 3. Describe the stages in volcano formation.
The cause of it all… What causes volcanoes to erupt???
BHS Earth and Space Science
What is a Volcano??? Volcanoes are often cone-shaped, but they can take other shapes too. They are formed when molten, sticky rock called magma, forces.
Volcanoes Chapter 9 Sections 1,2 and 3 VOLCANOES.
The locations of volcanoes are mostly determined by plate tectonics.
Volcanoes Volcanic landforms.
Chapter 10-Volcanoes and Other Igneous Activity
Essential Question How do volcanoes shape the earth?
5.1 Volcanoes and Plate Tectonics
VOLCANOES.
10.1 The Nature of Volcanic Eruptions
Station #9: At this station you will:
copyright 2009 abcteach.com
Volcanoes.
Volcanoes.
Volcanoes.
Volcanoes.
The locations of volcanoes are mostly determined by plate tectonics.
Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries.
10.1 Types of Volcanoes Anatomy of a Volcano
Volcanoes and You.
Continuation of earth’s process part 2
Volcanoes.
Presentation transcript:

GG103 Nasir Gadzar

Mahukona Loihihi

Volcanoes Defined Types of Volcanoes Volcanoes of the island of Hawaii –Descriptions –Images Presentation Summary

Volcanoes Defined vol·ca·no n. pl., vol·ca·noes or vol·ca·nos. Abbr. vol. 1. a. An opening in the earth's crust through which molten lava, ash, and gases are ejected. b. A similar opening on the surface of another planet. 2. A mountain formed by the materials ejected from a volcano.

Types of Volcanoes Geologist categorize volcanoes into four groups. 1)Composite 2)Cinder 3)Shield 4)Lava domes

Composite Volcanoes Called “composite” because they are made of alternating layers of lava and rock. Oftentimes called “Stratovolcanoes” Physical Characteristics –Steep –Symmetrical cone shaped –Often have snowcapped tops –Explosive eruptions

Examples of Composite volcanoes Mount Ranier, Washington, USA Mount Fuji, Honshu, Japan

Cinder Volcanoes Simplest type of volcano Built from particles globs of coagulated lava expelled from a solitary vent which then falls and solidifies around the vent to form a circular cone. Physical Characteristics –Bowl shaped crater –Size is usually about 1000ft. The size of a hill. –Single vent

Example of Cinder cone volcanoe Parícutin volocano, Mexico

Lava domes Also known as “volcanic domes” Usually occur on flanks of composite volcanoes Formed by bulbous masses of lava too viscous to flow any great distance, eventually piles around vent and dome becomes bigger from acitivity within. Physical Characteristics –Rounded –Steep sided

Example of Lava dome Unzen lava dome, Japan

Shield Volcano Built almost entirely of fluid lava flows. Flow pours out in all directions from a central summit vent, or group of vents, building a broad, gently sloping cone of flat, domical shape, that profiles a warrior shield. built up slowly by the accretion of thousands of highly fluid lava flows called basalt lava that spread widely over great distances, and then cool as thin, gently dipping sheets. Lavas also commonly erupt from vents along fractures (rift zones) that develop on the flanks of the cone.

Shield Volcano facts 3-4 miles in diameter but heights of feet. The Hawaiian Islands are composed of linear chains of these volcanoes. Shield Volcanoes of the Island of Hawaii –Kilauea –Mauna Loa –Mauna Kea –Hualalai –Kohala

Southernmost shield volcano on the Big Island. Predominantly erupts basaltic lava in profuse eruptions. Kilauea stands just under 4200 feet tall at it's highest point. Kilauea has a 165m deep circular caldera at its summit that measures 3x5km.

At 60 miles long and 30 miles wide, it makes up half of the entire island. Mauna Loa is the largest active volcano in the world. The thickness of its lava pile from the center of the volcano from is 56,080 ft (17,170 m).

Tallest volcano on the Island of Hawaii. Tallest mountain in the world. From sea floor to summit it towers more than 5.6 miles (9 km). Mauna Kea is the only Hawaiian volcano known to be glaciated. The most recent eruption was about 3,500 years ago. Mauna Kea is considered a dormant volcano.

Cinder cone on top of Mauna Kea

The summit of Hualalai rises to an elevation of 2523m (8271ft) above sea level. Hualalai is well-known in Hawaii as a good source for mantle xenoliths. The surface of Hualalai is entirely composed of post-shield alkalic basalts. The last historical eruption at Hualalai ended in This eruption produced very fluid, high velocity lava flows that entered the ocean off western Hawaii. Presently, the volcano is mantled by alkalic lavas erupted during the post-shield stage of volcanism.

Summit elevation of 1700 m (5577ft.) Kohala is considered to be extinct because it has not erupted for 60,000 years. Kohala is the oldest of the sub-aerial volcanoes that make the Island Of Hawaii.

Volcanoes are openings in the earth's crust through which molten lava, ash, and gases are ejected. There are four categories of volcanoes 1) Composite 2) Cinder 3) Lava dome 4) Shield Volcanoes found in the island of Hawaii are Shield volcanoes, these volcanoes names are: Kilauea, Mauna Loa, Mauna Kea, Hualalai, and Kohala. Mahukona is a seamount in west.