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Megatsunami - SchoolNova
Megatsunami - SchoolNova

... Megatsunami is an informal term to describe a tsunami that has initial wave heights much larger than normal tsunamis. • Origin: a large scale landslide, collision, or volcanic eruption event as opposed to raising or lowering of the sea floor due to tectonic activity. ...
Google Earth Volcano Lab
Google Earth Volcano Lab

... In this lab, you will be visiting many different volcanoes. As we learned, there are 3 different types of volcanoes that can be classified in different ways. Each volcano is unique. For every volcano you see, you will be asked to find the following information: ...
Back
Back

... eruption that created a dangerous cloud of gas and pyroclastic flow that killed 29,000 residents within two minutes • Answer • Mt. Pelee ...
What is like living near a volcano?
What is like living near a volcano?

... • Locals economies can profit from volcanism throughout the year, whereas skiing, for example, has only a limited winter season. • In Uganda, a country trying hard to increase its tourist industry, the volcanic region around Mt Elgon is being heavily promoted for it's landscape, huge waterfalls, wil ...
Powerpoint Presentation Physical Geology, 10/e
Powerpoint Presentation Physical Geology, 10/e

... reaches Earth’s surface • Explosive eruptions can produce rapidly cooled rock fragments called pyroclasts – Size range from dust (ash) to boulders (blocks and volcanic bombs) ...
Earth Science Chapter 6 Volcanoes
Earth Science Chapter 6 Volcanoes

... the Earth’s surface – Lava: molten rock that has reached the Earth’s surface – Magma Chamber -magma collected inside a volcano pocket – Pipe - a long tube that connects the magma chamber to Earth's surface. – Vent - an opening through which the magma leaves the volcano – Crater - a bowl-shaped area ...
RNDr. Aleš Špičák, CSc. - Sopečná činnost
RNDr. Aleš Špičák, CSc. - Sopečná činnost

... in the crust. It heats up local rocks, which melt to form viscous, water-rich magmas. Three times in the past 2.1 million years, large batches of these magmas have erupted explosively, forming huge calderas. ...
Volcanoes
Volcanoes

... – Tephra: Rock and hardened lava that pops/explodes out of ...
Volcanoes 22.6
Volcanoes 22.6

... Lava flow = stream of low viscosity lava Lava flows can travel great distances Pahoehoe = HOT, fast moving lava, ropelike surface • Aa = cooler, slow-moving lava, crumbly appearance ...
Volcanic Activity
Volcanic Activity

... • Lots of pyroclastics • Killed the Krafts and Harry Glicken, a survivor of Mt. St. Helens • Site of volcano warning system 1991 - 43 scientists and journalists were killed by a three-mile-long pyroclastic flow, a fast-moving river of hot gas and rock that can speed along at speeds up to 450 miles p ...
Lecture 04 Volcanic Activity g
Lecture 04 Volcanic Activity g

... composite volcano (prior to eruption) ...
Volcanoes lesson 2
Volcanoes lesson 2

... collapse of an ancient volcano, posthumously named Mount Mazama. This volcano violently erupted approximately 7700 years ago. The basin was formed after the top 5000 feet of the volcano collapsed. Subsequent lava flows sealed the bottom, allowing the caldera to fill with approximately 4.6 trillion g ...
VOLCANOES
VOLCANOES

... • Hawaiian volcanoes progress through pre-shield Lōʻihi, shield Mauna Loa and Kīlauea, post-shield Mauna Kea, Hualālai, and Haleakalā, erosional Kohala, Lāna‘i, and Wai‘anae, and rejuvenated Ko‘olau and West Maui stages. • As the islands age, they erode and subside, becoming atolls and seamounts. ...
volcanoes - an-0001
volcanoes - an-0001

... • This also affects the surrounding landscape and its people. • Pompeii was buried by the eruption and killed more than 2,000 people. • Pompeii was buried for over 1500 years. ...
What are Volcanoes?
What are Volcanoes?

... and gases shoot out from the volcano, often at supersonic speeds. Instead of lava these volcanoes blow molten rock into the air where it will harden. The larger pieces fall to the Earth and the smaller portions can circle the globe for years in the upper atmosphere. ...
Volcanoes
Volcanoes

... • The ash-cinder volcano: throws out (in addition to lava) much ash into the air. Through this the volcanic cone is built up from alternate layers of ash and cinder. ...
The Restless Earth Revision - Geography
The Restless Earth Revision - Geography

... Yellowstone National Park - Is one of the largest supervolcanoes in the world. Scientists have revealed that it has been on a regular eruption cycle of 600,000 years. The last eruption was 640,000 years ago... so the next is overdue. ...
lecture04r
lecture04r

... silica, andesitic magma. gases are trapped in the magma. When it erupts out onto the surface, low pressure causes dissolved gases to come out of solution just as the lava is freezing. The lava explodes, Resulting in a nuee ardente. ...
H.Albert et al.
H.Albert et al.

... crystals of the Siete Fuentes, Fasnia and Arafo eruptions (Albert et al., 2015) shows that there ...
Ch 8: Study Guide - LWC Earth Science
Ch 8: Study Guide - LWC Earth Science

... 16. Hypothesizing Large volcanic eruptions eject large amounts of gas, dust, and ash into the atmosphere. This volcanic material can affect the world’s climate by blocking incoming solar radiation. An eruption from what type of volcano is most likely to cause global climate changes? Explain your ans ...
volcanoes 1 - Earth Science Teachers` Association
volcanoes 1 - Earth Science Teachers` Association

... volcano such as a steep cone, a broad shield volcano, a caldera (large crater-like basin at the top). They could also add features such as woodland, river valleys or houses onto the slopes of the volcanoes or close by to see which areas may be most affected in the event of an eruption. Investigate t ...
Earthquakes and Volcanoes
Earthquakes and Volcanoes

... blown into the air. Narrow bases with steep sides due to loosely arranged cinder type eruptions. ...
Lecture 12
Lecture 12

... and ashfall deposits. ...
Shield volcanoes
Shield volcanoes

... ash and lava (much more than normal volcanoes) 2) A thick cloud of super-heated gas and ash will flow at high speed from the volcano, killing, burning and burying everything it touches. Everything within tens of miles will be destroyed. 3) Ash will shoot kilometres into the air and block out almost ...
PDF file of Chapter 5 lecture - Volcanoes
PDF file of Chapter 5 lecture - Volcanoes

... Large, cone-shape volcano (1000s ft. high & miles wide at base) Most next to Pacific Ocean in “Ring of Fire” (e.g., Fujiyama, Mt. St. Helens) Alternating lava flows and layers of pyroclastic debris Most violent type of activity (e.g., Mt. Vesuvius) ...
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Mount Pinatubo



Mount Pinatubo (Filipino: Bundok Pinatubo) is an active stratovolcano in the Cabusilan Mountains on the island of Luzon, near the tripoint of the Philippine provinces of Zambales, Tarlac, and Pampanga. Before the volcanic activities of 1991, its eruptive history was unknown to most people. It was heavily eroded, inconspicuous and obscured from view. It was covered with dense forest which supported a population of several thousand indigenous people, the Aetas, who fled to the mountains during the Spanish conquest of the Philippines.The volcano's Plinian / Ultra-Plinian eruption on 15 June 1991 produced the second largest terrestrial eruption of the 20th century after the 1912 eruption of Novarupta in the Alaska Peninsula.Complicating the eruption was the arrival of Typhoon Yunya (Diding), bringing a lethal mix of ash and rain to areas surrounding the volcano. Successful predictions at the onset of the climactic eruption led to the evacuation of tens of thousands of people from the surrounding areas, saving many lives, but the surrounding areas were severely damaged by pyroclastic flows, ash deposits, and subsequently, by the lahars caused by rainwaters re-mobilizing earlier volcanic deposits causing extensive destruction to infrastructure and changing the river systems months to years after the eruption.The effects of the eruption were felt worldwide. It ejected roughly 10,000,000,000 tonnes (1.1×1010 short tons) or 10 km3 (2.4 cu mi) of magma, and 20,000,000 tonnes (22,000,000 short tons) SO2, bringing vast quantities of minerals and metals to the surface environment. It injected more particulate into the stratosphere than any eruption since Krakatoa in 1883. Over the following months, the aerosols formed a global layer of sulfuric acid haze. Global temperatures dropped by about 0.5 °C (0.9 °F) in the years 1991-93, and ozone depletion temporarily increased substantially.
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