The Nature of Volcanic Eruptions

Slides:



Advertisements
Similar presentations
CH The Nature of Volcanic Eruptions Roots: Dyn = energy (dynamic) Dys = bad (dysfunction) e- = away (eject) Ego = self (egotistic) Em = cover with.
Advertisements

The Nature of Volcanic Eruptions
A Brief Introduction tch?v=uZp1dNybgfc&edufilter=w EVLZJ6d7xNxQz8CLNMG2g&safe =active.
The Nature of Volcanic Eruptions
© 2011 Pearson Education, Inc. Earth: An Introduction to Physical Geology, 10e Tarbuck & Lutgens.
Chapter 5 Volcanoes and Volcanic Hazards. The Nature of Volcanic Eruptions  Factors determining the “violence” or explosiveness of a volcanic eruption:
Making Connections with New Stuff 1. 3 types of volcanoes 2. Volcanoes and the formation of Early Earth 3. Minerals, Rocks, and the Rock Cycle 4. Divergent.
Today: Chapter 6 Volcanism
10.1 The nature of volcanic eruptions
Volcanoes Chapter 10.
Types of Volcanoes and Volcanic Hazards
1.Crater– bowl-shaped formation at the top of a volcano.
Volcanoes. A volcano is a mountian that forms when molten rock (magma) is forced to the earth’s surface.
Parts of a Volcano 1. Gas emission: various gases such as CO2, H2O, nitrogen, and lesser gases such as chlorine, hydrogen, and argon. 2. Crater: depression.
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.
Earth Science 10.2A The Nature of Volcanic Eruptions
Volcanoes Geology 12 Citadel High School. What comes out of a volcano? Gas Most common: H 2 O - water CO 2 – Carbon Dioxide SO 2 – Sulfur Dioxide HCl.
Volcanoes and Other Igneous Activity
Warm-upWeek 14Day 1. Anatomy of a Volcano 1. Fissure (crack) in crust 2. Magma rises toward surface 3. Deposits igneous rock around VENT Volcano Mountain.
Volcano Notes. Anatomy of a volcano magma chamber pipe vent/crater lava tephra.
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.
Warm-up#49Apr. 3 May 18, 1980 – Mount St. Helens erupted with tremendous force –Blew off the entire north flank of the mountain –Ejected a cubic km of.
Igneous Activity. The Nature of Volcanic Eruptions Factors that determine whether a volcano erupts explosively or gently –Magma’s composition –Temperature.
Volcanoes. Parts of a Volcano magma chamber: a large reserve of magma that collects deep underground central vent: long tunnel which lava is pushed through.
Volcanoes. l Evidence that we live in an active planet l The gods of the underworld l Millions of people live near active volcanoes –The greatest geological.
Do Now: 1.What is convection? 2.In which layer does convection take place? 3.What is the heat source for convection? 4.Which layer makes up the tectonic.
Chapter TWELEVE Volcanoes.
Shield Volcanoes Basaltic Lava – low silica content, low viscosity, low gas content Hot spots – magma moves up from lower mantle and plates move over it.
Volcanoes Day 1 October 6, Objectives I will be able to identify what makes _______ _____________________________________ I will be able to compare.
Volcanic eruptions Factors that determine the violence of an eruption
Presented by Rana Faizan Saleem Roll.No (10)  Volcanoes  Structure of a Volcano  Volcanism and its Types  Types of Volcanoes  Landforms from Lava.
Volcanoes! Chapter 10.
Volcanoes and Igneous Features. Volcanic eruptions  Factors that determine the violence of an eruption Composition of the magma Temperature of the magma.
Volcanic Eruptions. Mafic Lava  Dark colored  Rich in magnesium and iron  Formed from oceanic crust  Cools rapidly.
Map of Volcanoes around the WORLD!. Volcano Discovery ea ea This site.
Volcanoes.
VOLCANOES ERUPTING MOUNTAINS. VOLCANOES What is a volcano? What is a volcano? A volcano is a mountain caused by erupting lava from the mantle. A volcano.
VOLCANOES.
VOLCANOES CHAPTER 10. Viscosity – the resistance to the flow. As temperature decreases, viscosity increases. As silica content increases, viscosity increases.
Volcanoes Chapter How & Where Volcanoes Form Sec. 1 What is a volcano? –1. opening in Earth’s crust through which molten rock (magma), gases, &
THE NATURE OF VOLCANIC ERUPTION
10.1 The Nature of Volcanic Eruptions
Volcanoes and Other Igneous Activity. The Nature of Volcanic Eruptions  Factors determining the “violence” or explosiveness of a volcanic eruption: 
Section 10-3 Explain the 2 factors that determine whether a volcanic eruption will be explosive or quiet. Describe the 3 basic forms that a volcano can.
Chapter 10 Volcanoes.
Ag. Earth Science Ms. Weigel
Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Students know: two kinds of volcanoes, one with violent eruptions.
NATURE OF VOLCANIC ERUPTIONS.
Volcanoes. Ag Earth Science – Chapter 10.1 viscosity A measure of a fluid’s resistance to flow.
Landforms from lava Lesson 3 part 1.
Chapter 10 Volcanoes.
10.1 – The Nature of Volcanic Eruptions
2012 Anak Krakatau Eruption in Indonesia
Chapter 10-Volcanoes and Other Igneous Activity
Volcano and Mountain Activities
The Nature of Volcanic Eruptions
OBJECTIVES: Types of Magma Anatomy of a Volcano Types of Volcanoes
Prentice Hall EARTH SCIENCE
Nature of Volcanic Eruptions
10.1 The Nature of Volcanic Eruptions
Volcanoes.
Chapter 10 Volcanoes.
Nature of Volcanic Eruptions
Volcanoes.
10.2 The Nature of Volcanic Eruptions
Nature of Volcanic Eruptions
Why do I always take the time to read these when all I do is wonder why I read these …. And now I’m reading this again! Geez … there I go, reading this.
Volcanoes Earth Science Chapter 10.
10.1 Types of Volcanoes Anatomy of a Volcano
Volcanic Eruptions Factors that determine the violence of an eruption Composition of the magma Temperature of the magma Dissolved gases in the magma.
Presentation transcript:

The Nature of Volcanic Eruptions Chapter 10, Section 1

Factors Affecting Eruptions The primary factors that determine whether a volcano erupts violently or quietly include magma composition, magma temperature, and the amount of dissolved gases in the magma Viscosity – a substance’s resistance to flow Something that is more viscous flows more slowly; as a lava flow cools, it becomes more viscous as the lava slows down The more silica there is in a lava, the more viscous that lava is During explosive eruptions, the gases trapped in magma provide the force to eject molten rock from the vent, an opening to the surface

Factors Affecting Eruptions

Volcanic Material The less silica content there is in a basaltic lava, the faster it will flow, lava flows are common in Hawaii Magma contains varied amounts of dissolved gases held in the molten rock by confining pressure, it only is about 1 to 6 percent of the total weight of the magma It is important to study the composition of volcanic gases, because they are the gases that formed the atmosphere in the past Pyroclastic material – name given to particles produced in volcanic eruptions The fragments ejected during eruptions range in size from very fine dust and volcanic ash (less than 2 millimeters) to pieces that weigh several tons (blocks and lava bombs)

Volcanic Material

Concept Check What is a volcanic bomb? A large streamlined chunk of pyroclastic material that is larger than 64 mm in diameter.

Anatomy of a Volcano The three main volcanic types are shield volcanoes, cinder cones, and composite cones Volcanic activity often starts with a fissure, or crack, develops and magma is forced through it Volcano – a mountain built by repeated eruptions of lava or pyroclastic material often separated by long inactive periods Crater – steep-walled depression located at the top of many volcanoes The form of the volcano is largely determined by the composition of the magma

Anatomy of a Volcano

Shield Volcanoes Shield Volcano – produced by the accumulation of fluid basaltic lavas Shape – broad, slightly domed structure that resembles a warrior’s shield Most have grown from the ocean-floor to form islands (Hawaii and Iceland)

Shield Volcanoes

Cinder Cones Cinder Cone – built by ejected lava fragments the size of cinders, which harden in the air Product of relatively gas-rich basaltic magma Shape – determined by the steep-sided slope that loose pyroclastic material maintains as it comes to rest Usually the product of a single eruption that lasts only a few weeks, rarely a few years The magma in the pipe solidifies after the eruption, and the volcano doesn’t erupt again Cinder cones are small, ~30-300 meters and less than 700 meters in height There are thousands of cinder cones around the world

Cinder Cones

Composite Cones Composite Cone (Stratovolcano) – large, nearly symmetrical structure composed of layers of both lava and pyroclastic deposits The silica-rich magmas typical of composite cones generate viscous lavas that can only travel short distances May generate the most explosive eruptions that eject huge quantities of pyroclastic materials About 50 of these have erupted in the U.S. in the last 200 years The most dangerous results of one of these eruptions is a pyroclastic flow (hot gases and rock fragments), coming at a speed of 200 km/hr Lahars – destructive mudflow created when volcanic debris becomes saturated with water and rapidly moves down the volcano, often following stream valleys

Composite Cones

Concept Check What is a lahar? A mudflow down the slope of a volcano.

Profiles of Volcanic Landforms

Other Volcanic Landforms Caldera – a large depression in a volcano Forms by: (1) collapse of the top of a composite volcano after an explosive eruption, or (2) collapse of the top of a shield volcano after the magma chamber is drained Most volcanoes are fed magma through conduits, called pipes, connecting a magma chamber to the surface When the volcano has been eroded, especially cinder cones, the harder solidified magma will remain and become a volcanic neck Lava Plateau – the greatest volume of volcanic material doesn’t build volcanoes, but is extruded through fissures and flows over a large area

Formation of Crater Lake, Oregon

Volcanic Areas in the Northwestern United States

Assignment Read Chapter 10 Chapter 10 Assessment