Section 1 - kjpederson
... 5. magma chamber: the pocket beneath a volcano where magma collects 6. pipe: a long tube through which magma moves from the magma chamber to Earth’s surface 7. pyroclastic flow: the expulsion of ash, cinders, bombs, and gases during an explosive volcanic eruption 8. vent: the opening through which m ...
... 5. magma chamber: the pocket beneath a volcano where magma collects 6. pipe: a long tube through which magma moves from the magma chamber to Earth’s surface 7. pyroclastic flow: the expulsion of ash, cinders, bombs, and gases during an explosive volcanic eruption 8. vent: the opening through which m ...
mount st helens presentation byme nd rachael welton
... feet (24,400m) into the sky. • At the same time, ice, snow and several glaciers which were on the volcano melted forming a large series of lahars that reached as far as the Columbia River ( nearly 50 miles to the south west) ...
... feet (24,400m) into the sky. • At the same time, ice, snow and several glaciers which were on the volcano melted forming a large series of lahars that reached as far as the Columbia River ( nearly 50 miles to the south west) ...
Igneous Bodies: Intrusives
... • 1. Composite/Strato: composed of layers of pyroclastics and lava flows – Andesitic rock usually (intermediate lava) – Ex. Mt. Baker, Mt. Vesuvius, Mt Fuji ...
... • 1. Composite/Strato: composed of layers of pyroclastics and lava flows – Andesitic rock usually (intermediate lava) – Ex. Mt. Baker, Mt. Vesuvius, Mt Fuji ...
Student Science Volcano Project
... The magma rises through holes in the Earths crust called vents. Once the magma flows onto the Earths surface, it is called lava. Magma that erupts as fragments of molten material that solidify in the air is called pyroclastic material. Pyroclastic material includes magma and fragments of rock that a ...
... The magma rises through holes in the Earths crust called vents. Once the magma flows onto the Earths surface, it is called lava. Magma that erupts as fragments of molten material that solidify in the air is called pyroclastic material. Pyroclastic material includes magma and fragments of rock that a ...
Volcano Types (39)
... becomes enriched in silica • Silica-rich granitic magma is thick, and gas gets trapped inside, causing pressure to build up ...
... becomes enriched in silica • Silica-rich granitic magma is thick, and gas gets trapped inside, causing pressure to build up ...
Volcano Lesson Plan - Disaster Resilience Education For Schools
... volcanic eruptions occur and how to stay safe during an eruption. ...
... volcanic eruptions occur and how to stay safe during an eruption. ...
Unit 3 Section 2 Volcanoes Answer Key - WAHS
... A composite cone forms by many eruptions of material with medium or high-silica content. They erupt violently when pressure builds up in the magma. After the initial explosion, lots of gooey (viscous) lava oozes out of the top. The volcano becomes quiet for a while, but pressure builds and repeats t ...
... A composite cone forms by many eruptions of material with medium or high-silica content. They erupt violently when pressure builds up in the magma. After the initial explosion, lots of gooey (viscous) lava oozes out of the top. The volcano becomes quiet for a while, but pressure builds and repeats t ...
iss__st4_files/Comenius Volcanoes
... - Hawaiian - Hawaiian type eruptions are characterized by quiet ...
... - Hawaiian - Hawaiian type eruptions are characterized by quiet ...
Make a Volcano Lesson Plan - Purdue Extension
... Show 4-H Club members the principles of volcanic eruptions by creating a volcano (without the high temperature). 1. Place 3 to 4 tablespoons of baking soda into the glass jar. 2. Add a few drops of food coloring to ½ cup vinegar. Pour vinegar over the baking soda and watch it fizz. 3. You can also c ...
... Show 4-H Club members the principles of volcanic eruptions by creating a volcano (without the high temperature). 1. Place 3 to 4 tablespoons of baking soda into the glass jar. 2. Add a few drops of food coloring to ½ cup vinegar. Pour vinegar over the baking soda and watch it fizz. 3. You can also c ...
Make a Volcano Lesson Plan - Indiana 4-H
... Show 4-H Club members the principles of volcanic eruptions by creating a volcano (without the high temperature). 1. Place 3 to 4 tablespoons of baking soda into the glass jar. 2. Add a few drops of food coloring to ½ cup vinegar. Pour vinegar over the baking soda and watch it fizz. 3. You can also c ...
... Show 4-H Club members the principles of volcanic eruptions by creating a volcano (without the high temperature). 1. Place 3 to 4 tablespoons of baking soda into the glass jar. 2. Add a few drops of food coloring to ½ cup vinegar. Pour vinegar over the baking soda and watch it fizz. 3. You can also c ...
Earthquakes and Volcanoes
... Change in speed of S and P waves Small rise or fall of land near faults Changes in water levels in wells ...
... Change in speed of S and P waves Small rise or fall of land near faults Changes in water levels in wells ...
Homework04 n
... 2. A flow of mud and pyroclastic material is called a ________. 3. A volcanic dome forms when rising ________ cools and hardens within a volcano’s crater. 4. Pyroclastic materials that cool and solidify from lava ejected into the atmosphere are called _________. 5. When basaltic lava erupts beneath ...
... 2. A flow of mud and pyroclastic material is called a ________. 3. A volcanic dome forms when rising ________ cools and hardens within a volcano’s crater. 4. Pyroclastic materials that cool and solidify from lava ejected into the atmosphere are called _________. 5. When basaltic lava erupts beneath ...
Volcanoes and Igneous Activity Earth
... Frequently occur in groups Associated with subduction zones ...
... Frequently occur in groups Associated with subduction zones ...
Document
... into a grey, lifeless landscape. Now, twenty-two years later, the land around the mountain is slowly healing itself. Nature is covering the scars of the eruption but many people will never forget what happened that day. ...
... into a grey, lifeless landscape. Now, twenty-two years later, the land around the mountain is slowly healing itself. Nature is covering the scars of the eruption but many people will never forget what happened that day. ...
Compared to the desolate surface of the Moon, Earth must
... Can flow like basalt (effusive) or erupt explosively. More viscous, flows do not travel as far and generally thicker flows. ...
... Can flow like basalt (effusive) or erupt explosively. More viscous, flows do not travel as far and generally thicker flows. ...
ppt: volcano intro hook
... Understanding why material comes out of a volcano explosively in one spot and not at another is related to what’s happening under the surface ...
... Understanding why material comes out of a volcano explosively in one spot and not at another is related to what’s happening under the surface ...
Vocabulary Handouts
... molten rock. In modern times, scientists began to study volcanoes. They still don’t know all the answers, but they know much about how a volcano works. Our planet is made up of many layers of rock. The top layers of solid rock are called the crust. Deep beneath the crust is the mantle, where it is s ...
... molten rock. In modern times, scientists began to study volcanoes. They still don’t know all the answers, but they know much about how a volcano works. Our planet is made up of many layers of rock. The top layers of solid rock are called the crust. Deep beneath the crust is the mantle, where it is s ...
volcano powerpoint final
... mountain has erupted more than 50 times since the eruption in 79 A.D., when it buried Pompeii and its sister city, Herculaneum. After Pompeii was buried and lost to history, the volcano continued to erupt every 100 years until about 1037 A.D., when it entered a 600 year period of quiescence. The 79 ...
... mountain has erupted more than 50 times since the eruption in 79 A.D., when it buried Pompeii and its sister city, Herculaneum. After Pompeii was buried and lost to history, the volcano continued to erupt every 100 years until about 1037 A.D., when it entered a 600 year period of quiescence. The 79 ...
Earthquakes and Volcanoes
... is called lava. The place in the Earth’s surface through which magma and other materials reach the surface is called a volcano. In some places, lava can build up to forma cone-shaped mountain. • The opening from which lava erupts is the vent. Volcanoes often have more than one vent. ...
... is called lava. The place in the Earth’s surface through which magma and other materials reach the surface is called a volcano. In some places, lava can build up to forma cone-shaped mountain. • The opening from which lava erupts is the vent. Volcanoes often have more than one vent. ...
Lassen Volcanic National Park
... volcano. They are blobs and particles of congealed lava that is ejected from a single vent. When the lava is blown into the air it breaks into little pieces that solidify and fall as cinders around the vent to form an oval or circular cone. Composite volcanoes are mostly steep-sided, symmetrical con ...
... volcano. They are blobs and particles of congealed lava that is ejected from a single vent. When the lava is blown into the air it breaks into little pieces that solidify and fall as cinders around the vent to form an oval or circular cone. Composite volcanoes are mostly steep-sided, symmetrical con ...
Mount Edziza volcanic complex
The Mount Edziza volcanic complex is a large and potentially active north-south trending complex volcano in Stikine Country, northwestern British Columbia, Canada, located 38 kilometres (24 mi) southeast of the small community of Telegraph Creek. It occupies the southeastern portion of the Tahltan Highland, an upland area of plateau and lower mountain ranges, lying east of the Boundary Ranges and south of the Inklin River, which is the east fork of the Taku River. As a volcanic complex, it consists of many types of volcanoes, including shield volcanoes, calderas, lava domes, stratovolcanoes, and cinder cones.Most of the Mount Edziza volcanic complex is encompassed within a large provincial park called Mount Edziza Provincial Park. Named after Mount Edziza, this 2,660.95 km2 (1,027.40 sq mi) park was established in 1972 to preserve the volcanic and cultural treasures unique to the northern British Columbia area. The Mount Edziza volcanic complex is remote, and, without roads, accessible only along trails. The easiest access is from Highway 37 and a spur road from Dease Lake to Telegraph Creek. From Kinaskan Lake, on Highway 37, a poorly maintained trail extends west for 30 kilometres (19 mi) into the heart of the complex. From Telegraph Creek another trail extends east for 25 kilometres (16 mi) to the north slope of Mount Edziza.