v olcanoes chapter 11 section 11-2. v olcano the place where magma reaches the earth’s surface
TRANSCRIPT
![Page 1: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/1.jpg)
VOLCANOESChapter 11
Section 11-2
![Page 2: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/2.jpg)
VOLCANO
The place where magma reaches the Earth’s surface
![Page 3: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/3.jpg)
VENT
Vent - The opening from which lava erupts
![Page 4: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/4.jpg)
Crater – funnel shaped pit or
depression at the top of a volcano
cone
![Page 5: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/5.jpg)
4 MAJOR TYPES OF LAVA
Type 1 Dark colored Contains lots of
water Rich in iron and
magnesium When this lava
cools, igneous rocks such as basalt are formed
Type 2 Light in color Contains little water Rich in silicon and
aluminum Compounds of these
elements account for the light color
When this lava cools, it forms the igneous rock rhyolite
![Page 6: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/6.jpg)
4 MAJOR TYPES OF LAVA
Type 3 Chemical
composition close to the dark colored type and light colored type
Andesite is an example of the igneous rocks formed
Type 4 Contain large
amounts of gases such as steam and carbon dioxide
Forms rocks with many holes as lava cools because gas bubbles are trapped
Examples are Scoria and Pumice
![Page 7: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/7.jpg)
During volcanic eruptions, many rock fragments are blown in the air.
VOLCANIC DUST:• very fine• Less than .25 millimeter in diameter• Tiny as grains of flour
VOLCANIC ASH:• Particle size is between .25mm to 5
mm• 5 mm is the size of rice grains
VOLCANIC BOMBS:• Centimeter to a meter in size.• Cinders are volcanic bombs the size of
golf balls
![Page 8: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/8.jpg)
Types of Volcanoes
![Page 9: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/9.jpg)
Cinder ConesForm from explosive eruptions of rock particlesLow cone, narrow base, steep sidesParicutin, Mexico
Volcanoes that consist predominantly of pyroclastic materials are called cinder cones. These mountains, such as Capulin Mountain in New Mexico (USA), are easily eroded and usually do not reach great heights.
Types of Volcanoes
![Page 10: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/10.jpg)
Pyroclastic material is another name for a cloud of ash, lava fragments carried through the air, and vapor. Such a flow is usually *very* hot, and moves *rapidly* due to buoyancy provided by the vapors. Pyroclastic flows can extend miles from the volcano, and devastate life and property within their paths. Damage from pyroclastic flows can occur by impact of rock fragments moving at high speeds or burial of the surface with ash and coarser debris a foot or more thick. Hot pyroclastic surges may start fires and kill or burn people and animals. The most devastating pyroclastic flow occured during the eruption of Mt. Pelee in 1902.
![Page 11: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/11.jpg)
![Page 12: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/12.jpg)
![Page 13: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/13.jpg)
Shield VolcanoForms from quiet watery runny lava flow over large areaGently sloping dome shaped mountainsExample: Mauna, Hawaii
Shield volcanoes, on the other hand, are predominantly lava-based landforms that have gradual slopes and wide bases, because they release fluid lava slowly. These volcanoes can create huge landforms. Mauna Loa and Mauna Kea on the island of Hawaii (The Big Island) are classic examples: Mauna Kea has a base on the ocean floor more than 200 kilometres (120 miles) wide.
![Page 14: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/14.jpg)
Shield VolcanoForms from quiet watery runny lava flow over large areaGently sloping dome shaped mountainsExample: Mauna, Hawaii
![Page 15: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/15.jpg)
Composite VolcanoAlternating layers of rock particles and runny lavaViolent eruption first then quiet eruption that covers the rock particlesCone shaped mountainsMt. Fugi
![Page 16: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/16.jpg)
CalderaCrater, top of a volcano, that collapses or explodes to form a large pit
![Page 17: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/17.jpg)
Volcanic Activity• Volcanic activity is unpredictable• In order to indicate reactivity of volcanoes, scientist
classify them as either active, dormant, or extinct.
Active volcano• Erupts continually and periodically• An active volcano is a volcano that has had at least one
eruption during the past 10,000 years.
Dormant Volcano• A sleeping volcano• Known to have erupted in modern times• A dormant volcano is an active volcano that is not
erupting, but supposed to erupt again.
Extinct Volcano• Not known to have erupted in modern times but remain
unpredictable • An extinct volcano has not had an eruption for at least
10,000 years and is not expected to erupt again in a comparable time scale of the future.
![Page 18: V OLCANOES Chapter 11 Section 11-2. V OLCANO The place where magma reaches the Earth’s surface](https://reader035.vdocuments.mx/reader035/viewer/2022062804/5697bf721a28abf838c7eae5/html5/thumbnails/18.jpg)