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This volcano is not only known as Mt. Rainier but also as Tahoma, Tacobet, and Tacoma. If you wanna visit it's only 59 miles from Seattle and only 17 miles from the city Olympia. This was formed by the converging or the mashing together of Juan de Fuca and North America. This volcano is a cascade volcano which means   "an oceanic plate subducts underneath a continental plate."-anonymous, and cascade volcanoes are also a stratovolcano. Mt. Rainier was enlarged by layers of lava hardening as well as andesite and dacite. This volcano may be pretty but it's also deadly, for it is potentially the most dangerous known Cascade volcano "because of its great height, frequent earthquakes, active hydrothermal system, and extensive glacier mantle."-U.S Geological Survey. Though it hasn't erupted since 1894 you can never be too cautious, especially considering it had lava flowing, ash n the air, hot rocks, and gases coming out while causing an avalanche. It was mainly known to occur in the late 1800's, and it had erupted.

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This is a seduction area. one plate is slowly going over the other one while the other is going under and melting and basically getting recycled. It is a Basaltic Shield volcano. It has pyroclastic cone and lava domes. It has a quiet one where the lava just slowly comes out unless water gets into a vent. Basalt comes out of the volcano. it is by North Cascades National Park. And the Canada and USA border.
It was named after Sir James Clark's second ship. The last time the mountain erupted was over 1 million years ago.

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Kizimen is a stratovolcano in Kamchatka Russia. Kizimen has an elevation of 2,376 an is composed of layers of ash, rock and lava. This volcano formed at a subduction zone at a convergent boundary. This volcano formed about 12,000 years ago. The last time it erupted was January 10th, 2013. It shot up tons of ash and gas thousands of feet into the air. It is located near the town of Kamchatka in eastern Russia. There is no reports of Kizimen killing anyone. The eruptions are explosive and can be dangerous.

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Mount Fuji, Kitayama, Fujinomiya, Shizuoka, Japan

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Mount Fuji, Kitayama, Fujinomiya, Shizuoka, Japan

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Mount Fuji, Kitayama, Fujinomiya, Shizuoka, Japan

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The murian plate associated with the eurasian thetonic plate is causing the mount fuji form.
-convergent,
-it ownes its existence to the melting process.
-stratovolcano
-basalt
-frequent explosive eruptions.
-basaltic rock
-nobody lives there but there are nearby towns.
-(the legend) the tale goes that the mountain was born in a single day (1). The story relates the experiences of a woodsman named Visu. ... When he emerged from the doorway, he saw that the land near his home, which had been flat and dead, had become a mountain.
-The japanese serow and even black bears
-Volcano is considered and has erupte more than 15 times since 781
-december 16,1707
-72 houses and 3 buddhist temples were destroyed.

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Hekla
is a stratovolcano in the south of Iceland with a height of 1,491 m (4,892 ft). Hekla is one of Iceland's most active volcanoes; over 20. eruptions have occurred in and around the volcano since 874. During the Middle Ages, Europeans called the volcano the "Gateway to Hell".

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Pico ruivio is a Volcano situated  on Madeira Islands,in portugal it is  a stunning 1818 meters tall and this place can only be reached by foot
Elevation: 6,106′

Prominence: 6,109′

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Clear Lake Volcanic Field, California, USA

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Clear Lake Volcanic Field, California, USA

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Clear Lake Volcanic Field, California, USA

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between the Pacific and North American plate.
San Andreas transform system
cinder cone
lava
violent
Holocene
75,97
volcanic activity happened about 10,000 years ago
11,000
powerfully destructive

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cocos tectonic plates cause Pacaya volcano to create and form the volcano is formed by thee plates moving Stratovolcano The lava type is basaltic andesite strom

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cocos tectonic plates cause Pacaya volcano to create and form the volcano. formed by thee plates moving. Stratovolcano The lava type is basaltic andesite. strombolian type of eruption. tephra rock fragment spew out of the pacaya volcano. Guatemala city is where the pacaya volcano is located. The Pacaya Volcano is the largest post-caldera volcano. There is no life near the pacaya volcano. The pacaya volcano erupts almost once or twice a year. The pacaya has ruined peoples homes causeing them to have to evacuate.

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Mt. Kurikoma, Koeihigashi Kurikomanumakura, Kurihara, Miyagi, Japan

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Mt. Kurikoma, Koeihigashi Kurikomanumakura, Kurihara, Miyagi, Japan

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Mt. Kurikoma, Koeihigashi Kurikomanumakura, Kurihara, Miyagi, Japan

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-Most volcanoes in Japan are formed from magma originated in the mantle wedge. This magma is thought to be generated by the subduction of the oceanic plate.

-Kurikoma volcano is a convergentplate boundary.
-On land, volcanoes form when one tectonic plate moves under another. Usually a thin, heavy oceanic plate subducts, or moves under, a thicker continental plate.
-It is a complex stratovolcano volcano.   Tsurugi-dake lava dome is the lava to make it form..
-phreatic explosions is what the eruption produces.
-It is a hiking place.
-There is forest around the volcano.
-It started erupting 500,000 years ago.
-The last eruption was in 1944.
-The damage was lava went out of the volcano.

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Pavlof Volcano, Alaska, USA Brenden kidd

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Pavlof Volcano, Alaska, USA Brenden kidd

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the Pavlof  volcano

the Pavlof volcano is located in Alaska
the plates that cause this volcano to for is  the pacific plate
the convergent plate boundary created the volcano
north american plate is moving in a southern direction and pacific plate is moving northwest the lava is made of basaltic Andesite it has a explosive eruption that has a lot of ash that covers everything a nearby town is nelson lagoon the ash from the volcano covered the town with no warning of eruption and has erupted more that 25 times the last eruption was march 27 2016

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The volcano of Ollague is located in the Andes in Ollague, chile. That plates that cause Ollague to form are The Nazca plate and the South American plate. The volcano is located on a convergent boundary. Ollague was formed from the Nazca plate subducting under the South American plate.
The Ollague volcano is a stratovolcano with silicic lava flow with a summit didactic lava dome. There hasn't been a historical marking saying when the last eruption was or if it ever erupted. The types of rock fragments it sends out and is made of are Andesite ,  Basaltic Andesite, Dacite.
With in different distances there are small towns including a population of 27, 182, 1,246, and 17,574. Because the volcano hasn't erupted in the past 65,000 years no story's or legends have been made or told.
Life like near the volcano are dry and hot. That area has scarce rainfall. As you can imagine this place is a desert. As said before there hasn't been an eruption for a long time some people think that its extinct. While other think that it's just a dormant volcano waiting to erupt. So far no damage has occurred to anything nearby the volcano. However, the volcano itself is breaking down, there have been at least 3 flank collapses and few landslides.
This volcano seems as if it will break itself down before it erupts. Or it is just waiting for a big explosion.

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As one of the highest active volcanoes in the world, with a nearly perfect conical shape, Cotopaxi attracts more visitors than any other volcanoes in Ecuador. This is the classic volcano people imagine when they think of volcanoes. Cotopaxi is the second highest mountain in Ecuador and the most popular high altitude climb in the country because of the relative simplicity involved in the climb. But although, climbing Cotopaxi is considered not difficult, it is considered a technical climb too, because of the technical climbing gear necessary for the ascent, such as: crampons, ice axe and crevasse rescue gear. It is also known as the world’s third highest active volcano. In 1742, Cotopaxi erupted three times, destroying Latacunga and killing hundreds of people. The volcanic activity continues for the following 4 years. In 1768, Latacunga is destroyed again by another eruption killing many lives once more.

https://www.summitpost.org/cotopaxi/150311

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Arenal Volcano, Alajuela Province, San Carlos, Costa Rica

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Arenal Volcano, Alajuela Province, San Carlos, Costa Rica

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Arenal Volcano, Alajuela Province, San Carlos, Costa Rica

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Volcano Arenal is located at the bottom of mexico in a country called Costa Rico. This volcano was formed when the Cocos plate slid under the caribbean plate in a convergent plate  boundary. Volcano Arenal is a cinder cone volcano formed from Strombolian and Vulcarian tephra lava. Volcano Arenal is also a very quite but still dangerous volcano that shoot out basaltic andesite but oozes out Strombolian and Vulcarian tephra lava. Villages like San Luis and Tabacon live near volcano Arenal and life is not as bad as you would expect including all the rain you get, and how nice the weather always is even if you don't get snow. Volcano Arenal is most know for the massive eruption it had back in 1968 killing lots of people and destroyed tons of villages including livestock. This volcanoes last eruption was recently in 2010 but not as bad as it was back in 1968. Volcano Arenal was formed around 7000 years ago and only erupted once every 1000 years but now is started to erupt in a time a lot less then once every 1000 years.

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The santiaguito volcano is in guatemala on the caribbean plate which is a convergent boundary plate. These plates push together to make the stratovolcano form and it has dacitic lava. There was a eruptions of this volcano in 2011-2015 that were super violent and brutal but recently santiaguito eruptions have been gentle. What comes out of this volcano is super hot igneous rock fragments and some other rock particles. All guatemala mexico and honduras citizens towns can take damage from these volcanic eruptions. A cool thing about this volcano is it has been erupting every hour for the last 94 years. A recent eruption has reached over 7 kilometers (20,00+ feet). Life would not be fun near this volcano because it erupt almost every hour and has been for 94 years. The biggest eruption was in 1902 it is in the top 3 biggest eruptions and as a estimate about 6000 people died. August 24, 2016 was the last eruption and before that it was eruption about every hour. It has ruin towns and cities and has killed a lot of citizens of santa maria.

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this volcano's name is Reventador. it is located in Ecuador. it is located on the two plates named Nazca and South America. these two plates subducted to make this volcano.this volcano is a stratovolcano. the lava that comes out of this volcano is basaltic lava. this volcano is explosive and effusive.the rock that is formed from this volcano is andesited and tephra.this volcano is near villages and townes. it is farm land near the volcano.the history about the eruption is that its an ongoing eruption it is still erupting today.it started the ongoing eruption on march 30 2008.the last eruption that wasn't ongoing was march 30 2007.the damaged caused was just 2miles of ash piled up.

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Mount Ruapehu, Manawatu-Wanganui, New Zealand

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Mount Ruapehu, Manawatu-Wanganui, New Zealand volcano

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Mount Ruapehu, Manawatu-Wanganui, New Zealand volcano

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-cheyenne revard

Mount Ruapehu formed from the pacific plate under the indo-Australian plate.
The plate boundary creating the volcano is a convergent boundary.
How mount Ruapehu was formed was from subduction of the two plates.

Mount Ruapheu is a stratovolcano.
the type of lava that forms it is andesite lava.
The eruptions that Mount Ruapehu has had have been moderate and one time violent. With the most violent cause was a lahar that killed people in a railroad accident.
Andesite rock fragments mix with the lava of the volcano.

multiple towns live next to the volcano.
The legend of Mount Ruapehu is that Mount Ruapehu is a female mountain And its next to the next mountain Mount Taranaki which she is married to. Then one day when Mount Taranaki was away Mount Ruapehu was seduced by Mount Tongariruo. And so eventually Mount Taranaki left and went back to its original home.
Life like near the volcano is normal it has many attractions. But is still an active volcano and people should always be aware of it.
Mount Ruapehu's eruptions history is that it first erupted in 1895, 1945, 1995, 1996, and 2007.
Mount Ruapehu last erupted on September 25th 2007.
What happened from the last eruption was that drinking was contaminated, A lahar damaged a railway system and killed over 100 people.

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WHERE IS IT LOCATED?
the volcano is located in chile, south america.
WHAT PLATES CAUSE THE VOLCANO TO FORM?
the south american plates.
WHAT TYPE OF PLATE BOUDARY CREATED THE VOLCANO?
zazca plate.
WHAT ARE THE PLATES DOING CAUSING IT TO FORM?
converging.
WHAT KIND OF VOLCANO IS IT?
stratovolcano.
WHAT TYPE OF LAVA FROMS THE VOLCANO?
basltic-andesitic composition.
WHAT TYPE OF ERUPTION DOSE IS PRODUCE?
mild to moderate/ occasional lava.
WHAT TYPE OF VOLCANIC ROCK FRAGENTS OR LAVA COME OUT OF THE VOLCANO?
gas,lava, and fragmented debris (tephra)
WHO LIVES NEAR THE VOLCANO?
a town called villarrica.
LEGENDS OR STORIES ABOUT VILLARRICA?
there is a belif that instead of it being called snata maria magdaleana de villarrica the first conquares called it just villarrca.
WHAT IS LIFE LIKE NEAR THE VOLCANO?
They say its like living a normal like since the volcanos eruption isnt that deadly.
WHAT IS IT ERUPTION HISTORY?
It has had 61 eruptions its whole tie being active.
WHEN DID IT LAST ERUPT?
its most recent eruption was in 2020?
WHAT KIND OF DAMAGE OCCURRED?
not many because it is most surrounded by ice and snow and there is a pit of lava that catches it.

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Krakatoa is located in the USA in Illinois Mapleton.
The  Indian-Australian and Eurasian tectonic plates were the plates that caused Krakatoa to form.
Convergent plate boundary's were a part of how Krakatoa was created.
Molten rock from below rushes upward through this channel forming Krakatoa.
Krakatoa is a stratovolcano and a stratovolcano is a tall, conical volcano with multiple strata of solidified lava, tephra, as well as volcanic ash.
rhyolite is the type of lave that comes out of Krakatoa whenever it erupts.
Krakatoa has one of the most violent eruptions in history happening in 2020.
Krakatoa has very violent and frequent eruptions.
The city closest to Krakatoa is a city located about 100 miles west of Jakarta.
In august 1883 the eruption of Krakatoa killed more that 36,000 people making it one of the most devastating volcanic eruptions in human history.
Very few people live near Krakatoa but the people who do probably have a very bad experience with its eruptions.
Krakatoa seems to erupt every 100 to 200 years.
The last time Krakatoa erupted was in 2020 killing a lot of people.
As Krakatoa collapsed into the sea, it generated a tsunami 37m high – tall enough to submerge a six-storey building. And as the wave raced along the shoreline of the Sunda Strait, it destroyed 300 towns and villages, and killed more than 36,000 people.

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Isabela Island, Galápagos Islands, Ecuador

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Isabela Island, Galápagos Islands, Ecuador

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Isabela Island, Galápagos Islands, Ecuador

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Sierra Negra is a large shield volcano that was caused by a hotspot. Its eruptions are quiet. It is located in the Isabela Island in Ecuador. Its the largest volcano on the island. Its last eruption was in June of 2018 and before in October of 2005. There's a town nearby called Puerto Villamil.

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Fun Fact: Taal, Volcano has lake Taal inside of it

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In Progress. . .

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The cascade volcanoes were formed by the subduction of the Juan de Fuca under the North America plate. The tectonic plate boundary that formed it was the convergent plate boundary. When the volcano is forming, an oceanic plate subducts underneath a continental plate. The Cascade volcanic arc is a stratovolcano. The lava that formed this volcano is basaltic. The cascade volcanic arc has a quiet eruption.  About 7,765,004 people live in Washington state. In older times, people believed if rocks came out of the volcano, and they heard three whistles, the giants were coming. Near the volcano, the soil is fertile, but there is some volcanic rock laying around. Out of the whole volcanic arc, the last volcano to erupt was Mt. St Helens, in 1980. With that eruption, fifty-seven people were found dead, thousands of animals were killed, over 200 houses were destroyed, and over 185 miles of roads and railways were damaged.

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Lassen Peak, Lassen Volcanic National Park, California, USA

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Bella Scoglietti   Lassen Peak, Lassen Volcanic National Park, California, USA

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Bella Scoglietti   Lassen Peak, Lassen Volcanic National Park, California, USA

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Subduction plates. subduction plate boundary. one bends and slides underneath the other, curving down into the mantle. stratovolcano. rhyodacitic lava.explosive eruption. hybrid black dacite lava.Town.Lassen Park Ski Area grew from a single poma lift above the park highway in 1957 to include a chairlift, rope tows, and an A-frame chalet above and below the snow-covered park highway. One hundred years ago few people lived in the Lassen area; today a similar eruption would have a far more devastating effect on people's lives and the economy.The most recent eruptions in the Lassen area were the relatively small events that occurred at Lassen Peak between 1914 and 1917. The most recent large eruption produced Chaos Crags about 1,100 years ago. Such large eruptions in the Lassen area have an average recurrence interval of about 10,000 years. 1921. Partial collapse of the eruption column that fell onto the northeastern slope of Lassen Peak generated a high-speed flow composed of hot ash, pumice, rock fragments, and gas—called a pyroclastic flow—that swept down the side of the volcano, devastating an area of 3 square miles.

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Iwo Island, Iōjima, Ogasawara, Tokyo, Japan

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I s unusually flat and featureless for a volcanic island. Is the only obvious volcanic feature, as the island is only the resurgent dome (raised centre) of a larger submerged volcanic caldera surrounding the island.
The Mutsure-jima volcano is located in a island with no one there. This volcano has no erupted none during the past 10,000 years. And this volcano is extinct.
Type of Volcano: Shield Volcano
Type of Lava: Lava flow
Type of eruption: explosive and quiet
Type of volcanic rock: basalt

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Chaitén
The Chaitén volcano is in Chaitén, Chile.
Near the Gulf of Corcovado in southern Chile, and the city nearby is named Chiloé.
It formed from the Nazca plate beneath the South American Plate.
Chaitén is a caldera volcano.
Chaitén volcano erupted rhyolite magma unexpectedly and explosively on 1 May 2008.
Crackling with explosions, Chile’s Chaiten volcano began spitting lava on Tuesday following its first eruption in thousands of years.
Rhyolite magma often forms calderas, this being what formed Chaitén.
Puerto Aisen is the closet city to Chaitén.
May 2008, Chaitén volcano in Chilean Patagonia erupted and provided the world with spectacular footage of the first rhyolitic eruption ever to be observed in modern times.
there is often a lot of rain, lightning, and thunder.
Its most popular eruption is 2008, when it hadn't erupted in thousands of years.
The last eruption was 2011.
The Chaiten ash traveled as far as South Africa, and at least one aircraft encounter was reported. Ashfall can also cause damage to buildings and roads, disrupt power, and contaminate water supplies.

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oceanic plate seduction colliding strantovolcano andesitic violent basaltic andesite rhymesters 150 farm family a love story and that is why it erupts 8/14/15 is modern last was 1/24/16 1000 died and mud slid also avalanche

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Mount Norikura, Nyukawacho Iwaidani, Takayama, Gifu, Japan

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 Madison M - Mount Norikura, Nyukawacho Iwaidani, Takayama, Gifu, Japan

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 Madison M - Mount Norikura, Nyukawacho Iwaidani, Takayama, Gifu, Japan

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it is a convergent subduction volcano coming together. It is a stratovolcano volcano. the lava is a felsic lava. It is a violent volcano. since it is a stratovolcano volcano it kinda explodes. the rock fragments that come out of this volcano is Major Andesite / Basaltic Andesite Dacite. it is located on the borders of Gifu and Nagano prefectures in Japan. Bedouin legends say that Hala-'l-Bedr erupted fire and stones. people say it is characterized by rugged landforms dissected by deep river gorges. The highest peaks are found near the centre of the range. The eruption history is  early eruptions occurred at both the northern and southern ends of the present-day volcano, forming stratovolcanoes that have been largely buried by later southward-migrating eruptions. It last eruption took place about 2000 years ago. The damage it caused was power outages, drinking water .contamination, and wildfires.

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92. Orosi, coast rica, subduction beneath the Caribbean plate cause the volcano to form, convergent boundaries form the volcano by pushing towards each other.

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92. orosi is a inactive volcano which produces magma in a vilont eruption. and is basaltic, with about 8.3k people living nearby. It erupts when there people have upset the gods. pretty causious since when the volcano erupts it can be causious. its erupted since the 1800 all the way to 2021.  much damge occured like destruction of wildlife and homes. By: Nathan Hornsby

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Mount Canlaon, Negros Occidental, Philippines

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the ring of fire, convergent, they are crashing into eachother

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Mount Canlaon, Negros Occidental, Philippines

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Mount Canlaon, Negros Occidental, Philippines

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stratovolcano, phreatic,both, volcanic bombs,1,000 people, it is the Giant footstep of the warrior god , scary because you dont know if it is a earthquake or a eruption,

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Taupō, New Zealand
Pacific Plate
Destructive Boundary
Subduction Zone
Rhyolitic Volcano
Rhyolitic
Violent
Rhyolitic
26,000 people live here
Legend: A giant lizard man named Hotupuku lives near the volcano and eats any human that enters his home.
Eruption began 300,000 years ago
Last eruption was 1,800 years ago
A family friendly place with low crime rate
Lake outlets were blocked causing the water levels to rise by 34 meters.

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Nanzak Discus, Jalan Enau II, Pikgondeng, Condongcatur, Sleman Regency, Special Region of Yogyakarta, Indonesia

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Mount Ruapehu, Manawatu-Wanganui, New Zealand

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Mount Ruapehu, Manawatu-Wanganui, New Zealand

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Mount Ruapehu, Manawatu-Wanganui, New Zealand

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LOCATION:
The country it is located in is New Zealand. The city it is closest to is Ohakune.

TECTONIC PLATES:
It is caused by a subduction zone.
It is a subduction zone that created Mount Ruapehu.
The Pacific plate is going underneath the Australian plate.

TYPE OF VOLCANO:
It is a stratovolcano.
The type of lava is andesite lava.
It produces phreatic eruptions- they can be very explosive, which is violent.
Volcanic rock andesite will come from Mount Ruapehu.

EFFECTS OF THE VOLCANO:
There are a few towns/villiages near this volcano. They consist of Taumarunui, National Park villiage, Raetihi, Ohakune, Waiouru, and Whakapapa villiage.
Life near Mount Ruapehu is quite calm with the villiages and all, but sometimes it can send mudflow, ashfall, and sometimes even follow with eruptions.
Mount Ruapehu is one of the world´s most active volcanoes. Major eruptions include; 1895, 1945, 1995, 1996, and the most recent 2006.
It last erupted in 2006.
Since it´s in New Zealand, it has caused damages/ closures to 3 ski feilds with 100 million dollars in damages.

LEGEND:
There is a legend that says Mount Ruapehu was a female mountian and sat beside Tongariro, but was once wedded to Mount Taranaki. Taranaki was once away and Ruapehu was seduced by Tongariro, so that is why Ruapehu is now by him.

-Molly Young

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The Kookooligit Mountains are a volcanic mountain range on north-central St. Lawrence Island in the U.S. state of Alaska. They consist of a 30 km long and 40 km wide shield volcano capped with over 100 smaller volcanic cones.

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Divergent Plate Boundary...plates moving apart Eyjafjallajokull is a strato volcano The chamber derives magma from the tectonic divergence of the Mid-Atlantic r

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The Eyjafjallajökull volcano last erupted on 14 April 2010 in Iceland. The volcano has erupted relatively frequently since the last glacial period, most recently in 2010. Eyjafjallajokull consists of a volcano which is completely covered by an ice cap. On March 20, 2010 Eyjafjallajokull began spewing molten lava in an uninhabited area in south Iceland, after being dormant for 180 years. On April 14th, 2010, after a brief intermission, the volcano resumed erupting from the top crater in the center of the glacier. The renewed eruption caused massive flooding, which required an evacuation of 800 people. This second eruption threw volcanic ash several kilometers up in the atmosphere. The ash plume could be seen from miles away. That led to air traffic disruption in North-West Europe. The disruption lasted for six days, from April 15th to April 21st, that stranded thousands of travelers.

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Japan, Osaka, Sumiyoshi Ward, Bandai, 6 Chome−9−2 Ｖｏｌｋｓｗａｇｅｎ帝塚山

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Japan, Osaka, Sumiyoshi Ward, Bandai, 6 Chome−9−2 Ｖｏｌｋｓｗａｇｅｎ帝塚山

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Japan, Osaka, Sumiyoshi Ward, Bandai, 6 Chome−9−2 Ｖｏｌｋｓｗａｇｅｎ帝塚山

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Sinabung, Kuta Gugung, Karo Regency, North Sumatra, Indonesia

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Sinabung, Kuta Gugung, Karo Regency, North Sumatra, Indonesia

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Sinabung, Kuta Gugung, Karo Regency, North Sumatra, Indonesia

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Hot Spot no no plate boundary plates moving north

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Pahoehoe, Shield Volcano

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Bulusan Volcano, Irosin, Sorsogon, Philippines

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   mason jones   Bulusan Volcano, Irosin, Sorsogon, Philippines

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   mason jones   Bulusan Volcano, Irosin, Sorsogon, Philippines

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upon the NE rim of an older dacitic-to-rhyolitic caldera. are the plates that formed this volcano. type of boundary is convergent plate boundaries   divergent plate boundaries and convergent plate boundaries is why  it is formed. stratovolcano is the type of volcano. andesitic is the lava that forms my volcano. pancreatic explosions expound last in 1985. stratovolcano is the type of fragments. no one lives near it because it is an active volcano. it is very boring because you always have to be inside of if you are out side you have to wear a mask and gloves. the history of this volcano is it explodes a lot. the last erupts was 2016 on dec 29th. it could kill a lot of people by falling building

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its in the city of San Salvador. it is caused by subduction zone. the plate boundary is subduction. the plates are subducting. it is a Stratovolcano volcano. it has basaltic lava. violent. its near a city. no story or legend. human life is near it. it last erupted in 1917. a entire buisness section went up in flames.- Emma T

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Arenal, Alajuela Province, San Carlos, Costa Rica

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Arenal, Alajuela Province, San Carlos, Costa Rica

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Arenal, Alajuela Province, San Carlos, Costa Rica

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The volcano, Arenal, is most known for being a stratovolcano and is around 5,437. The volcano stands over much of the country side. In general, the Arenal area is safe to visit, though you still should use your common sense. Staying safe is the essential part of your trip. Costa Rica is the safest country in Central America, but it's always better to stay in tourist areas; furthermore, watch your surroundings and try not to flash your valuables. the youngest and one of the most active stratovolcano in Costa Rica. It is famous for a large explosive eruption in 1968 that killed several people and threw incandescent bombs to 5 km distance from the vent. The lake´s water is warm and fine for swimming but the most popular sports around are sailing, windsurfing and fishing for Guapote (bass), who put up fierce fight. it is not legal or safe to climb Arenal Volcano.

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Hoodoo Mountain, British Columbia, Canada

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Hoodoo Mountain, British Columbia, Canada

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Hoodoo Mountain, British Columbia, Canada

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Volcán Cotopaxi, Mirador 1ra Sección, Mexico City, CDMX, Mexico

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Volcán Cotopaxi, Mirador 1ra Sección, Mexico City, CDMX, Mexico

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Volcán Cotopaxi, Mirador 1ra Sección, Mexico City, CDMX, Mexico

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Cotopaxi is part of the Cordillera's Northern Volcanic Zone, the volcanism a product of the subduction of the Nazca Plate underneath the South American Plate. A convergent plate boundary is forming my volcano. The subduction of the Nazca plate underneath the South American plate. The Cotopaxi volcano is a Stratovolcano. The type of lava that forms my volcano is inter bedded blocky andesite lava. The eruption that Cotopaxi produced was a violent one. It erupted more than 50 times since 1738. It's eruptions often produced pyroclastic flows and destructive mud flows. The types of volcanic rock fragments that Cotopaxi produced are as follows, basaltic andesite, andesites and rhyolites. There are dozens of small farming communities at the southern foot of Cotopaxi. These isolated homes are far from the evacuation zones. A favorite legend is that of the battle between Taita Cotopaxi, a currently active volcano with a history of recent eruptions, with Taita Chimborazo, the highest mountain in all Ecuador, for the love of Mama Tungurahua, the most active volcano of them all. The story changes slightly depending on the people telling it. Residents who live near the volcano have grown used to living in a state of "yellow alert," the second scale on Ecuador's four-level warning system. They go about their days as Cotopaxi spits large volumes of ash and gas into the sky. Cotopaxi is among the highest active volcanoes in the world. Its most recent eruption began on August 14th, 2015, and ended on January 24th, 2016. Since 1738, Cotopaxi has erupted more than 50 times, resulting in the creation of numerous valleys formed by mud flows. Cotopaxi last erupted in August 2015. The explosions produced high eruptions columns, heavy ash fall, pyroclastic flows and lahars. The eruption caused much damage and there were fatalities.

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-Mayon is a is a subduction-zone volcano, forming above the subducting Philippine Sea Plate, which is sliding westwards, beneath the Philippines and the Sunda plate.
-It is a highly active stratovolcano, and consists mainly of 'A'ā augite-hypersthene-andesite (lava), generally fed from the crater. Mayon is very violent, one of the world's most active volcanoes. Pyroclastic rocks (porphyritic augite-hypersthene andesite) are frequently erupted from it.
-Many people live near this volcano, it supplies them with excellent farming opportunities and geothermal energy. “The way I kind of look at it is, the land doesn’t really belong to us. It belongs to Pele,” Sonner told the Post, referring to the Hawaiian volcano goddess. “We get to live on it while we can, and if she wants it back, she’ll take it. I have good insurance.” The eruptions displace many people who are living near Mayon, but denizens claim the risk is worth it. There have been more than 30 eruptions recorded since 1616. The most recent eruptive episode began in early January 2018 that consisted of phreatic explosions, steam-and-ash plumes, lava fountaining, and pyroclastic flows that repeatedly triggered large-scale evacuations. Mayon's most violent eruption, in 1814, killed more than 1200 people and devastated several towns.

-Gracie Julian

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Kabar, East Lombok Regency, West Nusa Tenggara, Indonesia

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The volcano Kaaba is located in Indonesia. This volcano is located next to Mount Hitam in the Bengkulu Province of Indonesia. The Arabian plates are causing this volcano to form, along with the transform plate boundaries. These plates are sliding past one another along the plate boundaries. Kaaba is a twin volcano with Basaltic and Pyroclastic flow lava erupting throughout. Kaaba is a historically active volcano with loud eruptions that have been erupting for many years. Pieces of dark rock and fragments cemented together are erupted out of it. There are villages located nearby, including Talang, Klingi and Bliti villages. In addition, there is also a nearby region including Summit. A popular historic story associated with Mount Kaaba includes the central summit craters, with explosions during the 19th and 20th centuries. Since this volcano is so active, there aren't a lot of people living nearby and live is lonely. In an 1833 eruption, it ejected water from the crater lake forming lahars that produced tons of damage to the nearby villages. The last eruption was in the year 2000 and the damage wasn't as major as the eruptions in the past years in the 1800's.

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Mount Agung, Jungutan, Karangasem Regency, Bali, Indonesia

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Mount Agung, Jungutan, Karangasem Regency, Bali, Indonesia

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Mount Agung, Jungutan, Karangasem Regency, Bali, Indonesia

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This volcano's Mount Agung. It is in Indonesia.  It is on the Sunda plate which is convergent.  It formed because it is on a subduction zone.  It is a stratovolcano and what formed from andesite lava.  It produces very violent eruptions.  when it erupts it produces andesite lava, volcanic breccia, volcanic ash, and pyroclastic debris.  The city of Bali live near it.  According to one Balinese myth, the deities made mountains for their thrones.  Its last eruption was in June 13, 2019 so people live normal but are prepared in case it happens again.  it sent an ash plume to 9.1 km altitude and threw hot rock up to 700 meters away.

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VolcanoChill, Alajuela Province, Poás, Costa Rica

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VolcanoChill, Alajuela Province, Poás, Costa Rica 

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VolcanoChill, Alajuela Province, Poás, Costa Rica 

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Poas, Costa Rica
Subduction from the Cocos tectonic plates - underneath the Caribbean Plate.
Convergent Plate Boundary is what is forming the Poas volcano.
The plates are colliding towards each other creating a convergent plate boundary which is what starts to form the Poas volcano.
stratovolcano
tephra, pumice and ash
violent eruptions
basaltic andesite lava
Cordillera Central - volcano is located in a national park
the story of the rualdo bird is tied to the poas volcano. The rualdo bird supposedly sings a song.
According to legend, a young tribal girl who lived near Poas Volcano befriended a rualdo bird when she was exploring the lush tropical rainforests nearby. The bird followed her everywhere, and the two became close friends.
Nobody necessarily lives near the volcano because it is inside of a national park in Costa Rica.
1914, 1915, 1916, 1925, and 1929, 1932-34.
Last erupted - September 30, 2019
explosions occured for several days in a row; destroyed lots of land surrounding it and also lots of land around or near the national park in which it was located in.

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the Llaima volcano is caused by a convergent boundary and subduction is what created the volcano, the volcano forms by the oceanic crust being pushed underneath the continental crust creating a subduction zone that formed the llaima volcano. it is an active stratovolcano with alternating layers of solidified ash, hardened lava and rock. when the llaima erupts it is violent. the eruption is visible even from as much as 45 miles away. the last time the volcano erupted 45 people were trapped inside a wilderness park, cut off from any means of escape. nobody was killed nor seriously injured from this incident. the longest eruption period for the llaima volcano was 1 year long, from 2008 to 2009. llaima volcano has over 40 flank vents that have formed cinder cones. llaima's first eruption was in early 1994 and has been the most active volcanoes in chile.

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Subduction of the North American Plate under the Caribbean Plate.
Subduction
a nuee ardente, a type of pyroclastic flow that consists of hot incandescent solid particles.
Stratovolcano
The lava is pasty
Violent
basic andesites and dacites
Saint Pierre
stories about mt. Pelee
If you were around mt. Pelee when it erupted you would be dead
Minor eruptions occured in 1792 and 1851 but it had a violent eruption in 1902
May 8, 1902
deaths of more than 29,000 people, as well as the nearly-complete destruction of the city of Saint Pierre by a single pyroclastic current, and is, sadly, the deadliest eruption of the 20th century.

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Irazú Volcano, Cartago Province, Costa Rica

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Irazú Volcano, Cartago Province, Costa Rica

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Irazú Volcano, Cartago Province, Costa Rica

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Irazu volcano
Irazu is located in Province, Costa Rica. subduction of the Pacific under the Carribean plate forms Irazu. Irazu is a stratovolcano, basalt and andesite lava forms inside of it. the eruptionin is very loud with a massive lava flow. not many villigaes and citys are by IRazu but there are some resturants near it. some believe the volcano was a gift for a gods daughter to be returned. the llast eruption was December 1994

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Mount Hood is a seemingly active volcano located in Oregon, where it towers over Oregon city. It was created by the convergent plates of Juan de Fuca and the North American plate. To make this volcano, the Juan de Fuca plate subducted beneath the North American. Mount hood was said to have formed anywhere from 500,000 years ago to 700,000, and is a stratovolcano, or made by layers of built up ash and basaltic andesite lava. This volcano does not have a past of being violent, but instead, lava flows out, only reaching about 6 to 8 miles away from the volcano. The last eruption of Mount hood was in September, 1865. This eruption lasted until January of 1866, leaving everyone in the area to evacuate as many mudslides would take place around the area after the eruption. People who live around the volcano pretty much continue normal lives, as if they didn't live near a volcano. The residents know the volcanoes history, and pay close attention to its volcanic activity, to know exactly what to expect. One myth or legend is that Mount Hood and Mount Adams were fighting over Mount Helens, leading them to fight and destroy villages in the process to gain her love.

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Mount Merapi, Dusun 2, Suroteleng, Boyolali Regency, Central Java, Indonesia

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Mount Merapi is a volcano in Indonesia located on the island of Java located near A town named Yogyakarta. This stratovolcano is risen up 9,551 and is the most active volcano in all of indonesia's 130 active volcanoes.

Mount Merapi has been active for 474 years ever since 1548 and the volcanoes latest eruption was just march 27th of last year! Mount Merapi was formed by convergent plate boundaries, by subduction around 400,000 years ago.

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Mount Agung, Jungutan, Karangasem Regency, Bali, Indonesia

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Mount Agung, Jungutan, Karangasem Regency, Bali, Indonesia

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Mount Agung, Jungutan, Karangasem Regency, Bali, Indonesia

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It is formed on a colliding plate boundary above the subduction zone where the Australian plate subducts underneath the Sudra plate.

It is a strata volcano and it's eruption is very violent and spews andesite lava, volcanic breccia, volcanic ash, and pyroclastic debris when it does.

Some Villages/Towns around the volcano are Amed, Kubu, Tista, Mahagiri, besakih, Ubud, Kuta, Seminyak, and Canggu.

In 2017(its most recent eruption), the volcano erupted and more than 140,000 people had to evacuate from their homes. Also in it's previous eruption in 1963, nearly 1,600 people died from it.

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Volcano Taal was formed by prehistoric eruptions between 140,000 and 5,380 BP

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Taal Volcano is located in the Philippians on a small island called Luzon. The volcano was formed by a subduction convergent boundary on the Eurasian plate. Taal was created because an oceanic crust and continental crust collided. It is a Caldera volcano, meaning it collapsed when it erupted. Taal has had countless violent eruptions often spewing basaltic lava or thick ash fall. Quezon and Taguig city are the near towns to the volcano. Despite many warning residents still decide to live there. Life near the Volcano is harsh. People often contract sickness from the volcanic smog causes sickness and irritation in the eyes. The last eruption was in 2021 on November 17th. Fortunately it was short lived and no one was hurt. Taal is the second most active volcano in the Philippines with over 30 reported eruptions in the last 448 years. The people of Philippines have an urban legend saying there was a princes named Taalita who lost her ring that her dad had given her. They had cherished the ring for generations. After weeks of searching a man had found it. The princess fell in love with him and they were soon married. One fateful morning they went on a boat ride and the princess dropped the ring in the ocean. She jumped in but didn't resurface. In a panic, the man did the same. After months of mourning an island with a volcano arose where they had died. The King named it Taal after his daughter.

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Santa Maria Quetzaltenango Department, Guatemala

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Santa Maria Quetzaltenango Department, Guatemala

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The Santa maria Volcano is located in Quetzaltenango, Guatemala. The plates causing this to form are the Coco's plate and the Caribbean plate, the type of plate boundary convergent and the coco's plate is sub-ducting under the Caribbean plate. It is a stratovolcano the type of lava that it forms is basaltic andesite, this volcano has very loud and explosive eruptions. The closest cities are Xela and Quetzaltenango. It has erupted a few times in the past, and the last time it erupted was August 22, 2013 and this volcano is still currently active It didn't cause to much damage.

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-Mayon is a is a subduction-zone volcano, forming above the subducting Philippine Sea Plate, which is sliding westwards, beneath the Philippines and the Sunda plate.
-It is a highly active stratovolcano, and consists mainly of 'A'ā augite-hypersthene-andesite (lava), generally fed from the crater. Mayon is very violent, one of the world's most active volcanoes. Pyroclastic rocks (porphyritic augite-hypersthene andesite) are frequently erupted from it.
-Many people live near this volcano, it supplies them with excellent farming opportunities and geothermal energy. “The way I kind of look at it is, the land doesn’t really belong to us. It belongs to Pele,” Sonner told the Post, referring to the Hawaiian volcano goddess. “We get to live on it while we can, and if she wants it back, she’ll take it. I have good insurance.” The eruptions displace many people who are living near Mayon, but denizens claim the risk is worth it. There have been more than 30 eruptions recorded since 1616. The most recent eruptive episode began in early January 2018 that consisted of phreatic explosions, steam-and-ash plumes, lava fountaining, and pyroclastic flows that repeatedly triggered large-scale evacuations. Mayon's most violent eruption, in 1814, killed more than 1200 people and devastated several towns.

-Gracie Julian

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85, Tondo, Manila, Metro Manila, Philippines

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85, Tondo, Manila, Metro Manila, Philippines

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85, Tondo, Manila, Metro Manila, Philippines

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Name: Sabancaya

Locations: its located in the Andes of southern Peru and it is northwest of a town called Arequipa.

What plates caused your volcano to form? The Nazca and South American plates.

What type of plate boundary is creating your volcano? Sabancaya is fueled by magma generated at the subduction zone and is a convergent plate.

Describe what the plates are doing that caused your volcano to form. Where the oceanic lithosphere of a tectonic plate converges with the less dense lithosphere of a second plate, the heavier plate dives beneath the second plate and sinks into the mantle.

What type of volcano is it?
stratovolcano
what type of lava forms your volcano?
a volcanic complex together with Hualca Hualca to the north and Ampato to the south and has erupted andesite and dacite. It is covered by a small ice cap which leads to a risk of lahars during eruptions.
what type of eruption does it produce?
it erupts andesite and dacite and it used to be very powerful but is less powerful now.
what types of volcanic rock fragments or lava come out of your volcano? andesite and dacite.

Who lives near sabancaya? nobody

fun fact: sabancaya means tongue of fire in the Quechua Indian language.

What is life like near sabancaya? there is no life near sabancaya.

Eruption history?  Historical reports indicate eruptions during the 18th century. The volcano returned to activity in 1986, culminating in a large eruption in 1990.

when did it last erupt? november 2018 and its still ongoing

what kind of damages occured? lahars

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Krakatoa, Anak Krakatau Island, South Lampung Regency, Lampung, Indonesia

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Krakatoa is located in Indonesia 100 miles west of Jakarta.
the Indian-Australian and Eurasian tectonic plates are the plates that have caused this volcano to form.
A convergent plate boundary is the boundary that created Krakatoa.
The plates that created Krakatoa have a lot of high volcanic and seismic activity.
Krakatoa is a stratovolcano and that means that they have steep sides and usually erupt frequently and violently.

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white island - M. Schöller & Schöller GbR, Obere Wässere, Reutlingen, Germany

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white island - M. Schöller & Schöller GbR, Obere Wässere, Reutlingen, Germany

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white island - M. Schöller & Schöller GbR, Obere Wässere, Reutlingen, Germany

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The White Island Volcano  is caused by a convergent boundary and a transform boundary is creating the volcano. The volcano forms by the land clashing and grinding together forming the White Island volcano. It is an active composite stratification. The lava that forms the volcano is Andesite lava. When the White Island volcano erupts it is violent. Volcanic rock fragments like Dacite lava flows and pyroclastic deposits come out of the volcano. A medicine man named Ngatoro was climbing up Tongariro with a woman named Auruhoe. ... They first came out of the water at White Island to see where they were, and the land burst into flames that are still burning. Twenty-seven of the 31 people injured in the eruption of the Whakaari/White Island volcano had burns to more than 30% of their body. The bodies of two victims have not been recovered and may have been lost to the sea. White Island was in eruption from December 1975 to September 2000, the longest and largest historic eruption episode. This eruption episode developed many collapse and explosion craters. For long periods active vents in these craters emitted volcanic ash. 9 December 2019. Casualties. The 47 people on the island at the time of the eruption consisted of 24 Australians, nine Americans, five Kiwis, four Germans, two Chinese, two Britons and one Malaysian.

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Location: Veracruz and Puebla, Mexico Mexico
The modern volcano was constructed during the late Pleistocene and Holocene of viscous andesitic and dacitic lavas.
Stratovolcano
highest mountain in Mexico and the third highest in North America, after Denali of Alaska in the United States and Mount Logan of Canada. Pico de Orizaba is also the highest volcanic summit in North America
Elevation: 18,491
Veracruz and Puebla, Mexico
According to the story, Nahuani was a brave woman who was always accompanied by her faithful eagle friend, Ahuilizapan, which means "Orizaba".

One day, Nahuani had to face one of the greatest battles and was defeated. Ahuilizapan, deeply disconsolate, rose to the highest point of the sky, dropping heavily to the earth.

In the place where she fell an enormous mountain began to form. With the passage of time, this mountain became a huge volcano.

Last eruption was in 1846

Type of lava felsic
dormant volcano
Pico de Orizaba is also the highest volcanic summit in North America. ... The volcano is currently dormant but not extinct, with the last eruption taking place during the 19th century. It is the second most prominent volcanic peak in the world after Africa's Mount Kilimanjaro.

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subduction of oceanic and continental crust 

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Convergent Boundary plates coming together
andesitic lava Strata Volcano
violent eruption and pyroclastic flows
400,000 people live nearby
Galeras is one of Colombia's most active volcanoes. In an eruption in 1993, it killed a group of scientists and tourists who had been inside its crater when it erupted.Travelers rest and relax in the 7,615 acre Galeras Volcano Wildlife Sanctuary’s cloud forest ecosystem. A watershed gives birth to about 125 streams, several rivers, and four lakes (Black, Green, Telpis, and Mejia). Six species of endangered frogs and 13 varieties of hummingbirds make their home in the sanctuary.

Last erupted in 2014

https://colombia.travel/en/pasto/galeras-volcano-wildlife-sanctuary