African+Plate+(17)

=__**African Plate**__=

Kilamanjaro - CS

 * World Map** (insert world map here) with citation (URL)

A typical eruption of a strato volcano is very explosive, usually involes blowing their top. http://www.skimountaineer.com/ROF/Beyond/Kilimanjaro/KilimanjaroMap2.jpg
 * Volcano Data**
 * Volcano Name: || Kilimanjaro ||
 * Location: || North east/Tanzania/3.07 S, 37.35 E ||
 * Tectonic Plate: || African Plate ||
 * Height: || 1,600 ft ||
 * Type of Volcano: || Stratovolcano ||
 * Rock type of lava: || unknown ||
 * Date of Last Eruption: || 150,000 years ago ||
 * Type of Last Eruption: || unknown ||
 * Detailed map** (insert detailed map here) with citation (URL)
 * Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL)
 * Topographic Map** (insert topographic map here) with citation (URL)

“Killimanjaro, Tanzania, japan.” Skimountaineer. KilimanjaroMap2 web. 16 nov. 2009.
 * Citations** for information in MLA style:

Kieyo - TM
Minor eruptions with lava that overran some cities. http://volcano.si.edu/world/volcano.cfm?vnum=0202-17=
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * Volcano Data**
 * Volcano Name: || Kieyo ||
 * Location: || Tanzania, 9.23 S, 33.78 E ||
 * Tectonic Plate: ||  ||
 * Height: || 2175m, 7,136 feet ||
 * Type of Volcano: || Strato volcano ||
 * Rock type of lava: ||  ||
 * Setting: ||  ||
 * Date of Last Eruption: || Around 1800 ||
 * Type of Last Eruption: ||  ||
 * Detailed map** (insert detailed map here) with citation (URL)
 * Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL)


 * Topographic Map** (insert topographic map here) with citation (URL)

Minor eruptions with lava that overran some cities. http://volcano.si.edu/world/volcano.cfm?vnum=0202-17=
 * Hazards:** (type your description below)


 * Citations** for information in MLA style:

Oku - AH
http://www.volcano.si.edu/world/volcano.cfm?vnum=0204-03- ||
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * Volcano Data**
 * Volcano Name: || Oku Volcano, Cameroon ||
 * Location: || 6°12'17.50"N 10°29'4.11"E ||
 * Tectonic Plate: || African Plate ||
 * Height: || 3011 meters (9880 feet) ||
 * Type of Volcano: || Strato volcano ||
 * Rock type of lava: || rhyolitic and trachytic ||
 * Setting: || Numerous maars and basaltic cinder cones lie on or near the deeply dissected rhyolitic and trachytic Mount Oku massif along the Cameroon volcanic line. The Mount Oku stratovolcano is cut by a large caldera. The Oku volcanic field is noted for two crater lakes, Lake Nyos to the north and Lake Monoun to the south, that recently produced catastrophic carbon-dioxide gas release events.
 * Date of Last Eruption: || Unknown ||
 * Type of Last Eruption: || Unknown ||
 * Detailed map** (insert detailed map here) with citation (URL)

Oku’s last eruption is. - UNKNOWN. Oku is a Strato Volcano. Also can be called composite cones. Strato Volcanoes have, huge bumps that stick out of the steep sides. The sides build up when the volcano erupts and lava, tephra and pyroclastic rock build up. It takes a long time almost thousands of years for the pressure to make the volcanos erupt. There is many types of rock and lave that build up on the sides. The types of magma on the strato volcanoes are, basalt, andesite, dacite and rhyolite. The magma causes explosive eruptions, but the only one that does not is basalt. Many vents are in strato volcanoes. Some are shapes as sinder canes and some are domes. Located low on the sides of the volcano. **Topographic Map** (insert topographic map here) with citation (URL) [] - information. www.pacificislandtravel.com/.../volcanoes1.gif -image.
 * Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL)

VOLCANO HAZARDS: Usually active volcanoes have hazards like huge lave flows, explosive blasts, volcanic eruptions. Others that are rarely noticed are glowing avalanches and ash falling but they can still be deadly. Some other hazards are rockslides and mudflows. http://www.cotf.edu/ete/modules/volcanoes/vhazards.html
 * Hazards:** (type your description below)
 * Citations** for information in MLA style:

Dubbi - LB
|| ** Latitude: ** || 13.58°N || 13°35'0"N || ||
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * Volcano Data**
 * Volcano Name: || Dubbi ||
 * Location: || Eritrea
 * ** Longitude: ** || 41.808°E || 41°48'30" ||
 * Tectonic Plate: || Divergent Arabian and African Boundary ||
 * Height: || 5,330 feet (1,625 m) ||
 * Type of Volcano: || [|Stratovolcano] ||
 * Rock type of lava: || Basaltic lava ||
 * Setting: || Boundary ||
 * Date of Last Eruption: || 1861 ||
 * Type of Last Eruption: || **Explosive** ||
 * Detailed map** (insert detailed map here) with citation (URL)
 * Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL) dubbi’s typical eruption is explosive dubbi last erupted in 1861 and it exploded dubbi can send huge clouds of smoke and ash into the air along with spewing lava the lava can flow all the way out to the red sea from where dubbi is. Dubbi was one of the most severe volcanic eruptions in all of Africa it erupted and took out 2 villages killing 100 people along with poisoning nearby areas with smoke and carbon dioxide and ash.

Dubbi’s last eruption was in 1861 so not many hazards are being taken, but dubbi can have lava flow all the way out to the red sea destroying anything in its path ash is also another hazard because dubbi is explosive it creates huge ash clouds that effect nearby villages.
 * Topographic Map** (insert topographic map here) with citation (URL)
 * Hazards:** (type your description below)

[] [] = http://www.earthtools.org/
 * Citations** for information in MLA style:

Karisimbi - AJF

 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * Volcano Data**
 * Volcano Name: || Karisimbi ||
 * Location: || **1.52 S, 29.43 E in Rwanda** ||
 * Tectonic Plate: || African Plate ||
 * Height: || **14,787 ft** ||
 * Type of Volcano: || Strato Cone ||
 * Rock type of lava: || Potassium-Argon ||
 * Setting: || Mid-East of the plate ||
 * Date of Last Eruption: || unknown ||
 * Type of Last Eruption: || unknown ||
 * Detailed map** (insert detailed map here) with citation (URL)
 * Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL)

It has a mediocre amount of silica so the amount of explosiveness doesn't have enough time to go very far without becoming hardened and way less dangerous.
 * Topographic Map** (insert topographic map here) with citation (URL)
 * Hazards:** (type your description below)

"Karisimbi, Rwanda." Web. 19 Nov. 2009. . "Rwanda Facts, information, pictures | Encyclopedia.com articles about Rwanda." //Encyclopedia - Online Dictionary | Encyclopedia.com: Get facts, articles, pictures, video//. Web. 19 Nov. 2009. .
 * Citations** for information in MLA style:

Google Earth Buyuda Volcanic Field - CM
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * Volcano Data**
 * Volcano Name: || = Bayuda Volcanic Field = ||
 * Location: || 18.33°N, 32.75°E Sudan ||
 * Tectonic Plate: || African plate ||
 * Height: || 2198 feet ||
 * Type of Volcano: || Cinder cones ||
 * Rock type of lava: || basalts ||
 * Setting: ||  ||
 * Date of Last Eruption: || unknown ||
 * Type of Last Eruption: || 850 AD ||
 * Detailed map** (insert detailed map here) with citation (URL)
 * Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL)


 * Topographic Map** (insert topographic map here) with citation (URL)
 * Hazards:** (type your description below)


 * Citations** for information in MLA style:

Nyamuragira - LHW

 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * Volcano Data**
 * Volcano Name: || Nyamuragira ||
 * Location: || Congo ||
 * Tectonic Plate: ||  ||
 * Height: || 3,056 ||
 * Type of Volcano: || Sheild ||
 * Rock type of lava: || Low viscosity ||
 * Setting: || Hotspot ||
 * Date of Last Eruption: || 2006 ||
 * Type of Last Eruption: || Low viscosity because low silica content ||
 * Detailed map** (insert detailed map here) with citation (URL)
 * Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL) The Magma is very low viscosity because it has a very low silica content. African volcanoes result from hotspots, the rifting in East Africa, or a combination of the two. The East African rift, one of the world's most dramatic extensional structures, has produced the continent's highest and lowest volcanoes, ranging from the massive Kilimanjaro to vents in Ethiopia's Danakil Depression that lie below sea level.


 * Topographic Map** (insert topographic map here) with citation (URL)
 * Hazards:** (type your description below) There are not hazards because the magma does not go very far and the volcanoe is not near a town


 * Citations** for information in MLA style: http://vulcan.wr.usgs.gov/Volcanoes/Africa/description_africa_volcanics.html

Marion Island - JP

 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * Volcano Data**
 * Volcano Name: || Marion Island ||
 * Location: || Mariana Is-C Pacific ||
 * Tectonic Plate: || Divergent ||
 * Height: || 4,035 feet ||
 * Type of Volcano: || Shield volcanoes ||
 * Rock type of lava: || Trachy Basaltic ||
 * Setting: ||  ||
 * Date of Last Eruption: || 2004 ||
 * Type of Last Eruption: || Gas and scoria ||
 * Detailed map** (insert detailed map here) with citation (URL)
 * Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL) The first eruption was going 5-km. This had also extended to the coast. This volcano erupts with gas and other objects. It has about three lava flows. The lava had poured of the cliffs about 50-70 meters high. Some lava had remained.

If there were people on this island they would be forced to move, to keep there lives. Marion Island is right in the middle of the ocean and not that far from South Africa, so it could cause a sunami. Some could be mixed with ash and travel a fast speed. A result of this is, is that people could get covered. Than there are others that are mixed with water, there speed is about 50 mph.
 * Topogrphic Map** (insert topographic map here) with citation (URL)
 * Hazards:** (type your description below)


 * Citations** for information in MLA style:

Kenya - RD
Found using: Google Earth Stratocone volcanoes are generally high in silica, and are very viscous, which causes the lava to explosively erupt. Mount Kenya, however, although it is a stratocone volcano, isn’t explosive, because it is mostly made of basalt rock, which is a rock low in silica. Due to the low silica, it is low in viscosity, causing it to ooze instead of explode. Mount Kenya is found on a divergent boundary, which generally yields low viscosity volcanoes. This geologic setting is reflective of Mount Kenya’s viscosity.
 * World Map** (insert world map here) with citation. Found using: Google Earth
 * World Map** (insert world map here) with citation. Found using: Google Earth
 * World Map** (insert world map here) with citation. Found using: Google Earth
 * World Map** (insert world map here) with citation. Found using: Google Earth
 * Volcano Data**
 * Volcano Name: || Mt. Kenya ||
 * Location: || Kenya, Africa ||
 * Tectonic Plate: || African Plate ||
 * Height: || 17,058 ft ||
 * Type of Volcano: || Stratovolcano (cone) ||
 * Rock type of lava: || Basalt ||
 * Setting: || Divergent plate boundary (of the African Plate) ||
 * Date of Last Eruption: || Between 2.6 and 3.1 million years ago ||
 * Type of Last Eruption: || Unknown ||
 * Detailed map** (insert detailed map here) with citation (URL)
 * Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL)
 * Topographic Map** (insert topographic map here) with citation (URL): []

Mount Kenya is not near enough to any city to create hazards in case of eruption, and hasn’t erupted in so long it is considered to be extinct. Because it is extinct, there are no safeguards and nothing/no one monitoring of the mountain. General hazards include altitude sickness, hypothermia, animal stampedes (mainly buffalo and elephant), dehydration, and getting lost. If it did erupt, Mt. Kenya could cause a very small lahar. This is because it has ice caps at its peak, yet due to global climate change, they have all but completely melted. There is still, however, the possibility of a lahar. The lava could be an issue because, as shown in the contour map, the mountain is steeper on the side closer to the city, which is southwest of the volcano. The city is still over 80 kilometers away though.
 * Hazards:** (type your description below)


 * Citations** for information in MLA style:

“Mt. Kenya, Kenya.” //Volcano World//. **Oregon** **State University**. Web. 15 Nov. 2009. []

“Mount Kenya.” //Volcano Live//. Web. 15 Nov. 2009. []

=**__Mt. Pico: NV__** = __**World Map**__:




 * Volcano Data:**
 * ====Volcano Name:==== || ====Mt. Pico==== ||
 * ====Location:==== || ==== 38.47°N   28.40°W  ==== ||
 * ====Tectonic Plate:==== || ====Unknown==== ||
 * ====Height:==== || ==== 2351 m  ==== ||
 * ====Type of Volcano:==== || ==== Stratovolcano  ==== ||
 * ====Rock type of lava:==== || ====Lava and Tepra==== ||
 * ====Setting:==== || ====Unknown==== ||
 * ====Date of Last Eruption:==== || ====1720==== ||
 * ====Type of Last Eruption:==== || ====Unknown==== ||

**Typical Eruption:**
====Mt. Pico’s eruptions are somewhat hazardous. In the last eruption, its explosive eruptions destroyed property and some homes of the local town’s people. Although the last eruption was almost 300 years ago, there was a volcanic eruption that was uncertain in 1963. But it is unconfirmed because it was a Submarine eruption.====

**Hazards:**
====Mt. Pico has explosive eruptions, so when it erupts it really erupts. And it is known for the damage upon the land, even in 1562(the first recorded data of this volcano) it was said to be very destructive.====

**Citations**:

 * ====[]====
 * ====[]====
 * ====[]====
 * ====[]====

[]
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * Volcano Data**
 * Volcano Name: || Atakor Volcanic Field ||
 * Location: || North Africa, Atakor Volcano Fields ||
 * Tectonic Plate: || African Plate ||
 * Height: || 9,573 feet ||
 * Type of Volcano: || Scoria/Cinder cones ||
 * Rock type of lava: || Basaltic ||
 * Setting: || Middle of the African plate ||
 * Date of Last Eruption: || unknown ||
 * Type of Last Eruption: || unknown ||
 * Detailed map** (insert detailed map here) with citation (URL)

I could not find the last known eruption or what is was like so I decided to just tell what a typical scoria/cinder cone volcano eruption is like. The magma in a cinder volcano has a high amount of silica. This causes gases to be trapped in the magma. These gases build up pressure and cause the magma to be pushed towards the surface of the earth. When the magma reaches the surface it explodes out of the top of the volcano in a violent manner. This can cause lahars and pyroclastic flows. Ash also is thrown into the air when this happens. Because the magma has a high level of silica content it doesn’t flow very far. When the lava hardens it won’t have flown very far so it will harden on the side of the volcano. This is why cinder volcanoes are steep and not very wide.
 * Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL)

None was available
 * Topographic Map** (insert topographic map here) with citation (URL)

When a volcano erupts there are five main dangers:
 * Hazards:** (type your description below)
 * 1) you could be covered by ash
 * 2) lava flow
 * 3) pyroclastic flow
 * 4) lahar

A pyroclastic flow is a mixture of ash and rock fragments mixed with hot gases. It has a high density. Pyroclastic flows only occur with explosive eruptions and move away from the volcano’s vents at speeds up to 220 miles per hour. Pyroclastic flows have two parts:
 * 1) the lower flow consists of coarse fragments that move along the ground
 * 2) the upper flow is a turbulent cloud of ash

The lower part of the flow follows the topography of the volcano down the side of the volcano. The flows are very destructive because they destroy everything in their path. Lahars are wet cement- like mixtures of water, mud and volcanic rock. Lahars flow down the side of volcanoes.


 * Citations** for information in MLA style:

http://www.volcano.si.edu/world/volcano.cfm?vnum=0205-005

Meidob Volcanic Field - JE
My volcanic field doesn’t have a volcano, so I can’t really tell you much about its eruption. For the most past the vents are the only active part of the field. However If it was to erupt then it would slowly ooze. So It would be a shield volcano.
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * Volcano Data**
 * Volcano Name: || Meidob Volcanic Field ||
 * Location: || Western, Sudan ||
 * Tectonic Plate: || African Plate ||
 * Height: || 2000 M ||
 * Type of Volcano: || Scoria cones, Lava domes, Maars ||
 * Rock type of lava: || ukknown ||
 * Setting: || convergent ||
 * Date of Last Eruption: || 5000 years ||
 * Type of Last Eruption: || Unknown ||
 * Detailed map** (insert detailed map here) with citation (URL)
 * Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL)


 * Topographic Map** (insert topographic map here) with citation (URL)


 * Hazards:** (type your description below) Meidob volcanic field is in the middle of nowhere so nothing really would be affected by the eruption. This eruption wouldn’t even make it out of the volcanic field there for people wouldn’t even anything happened.


 * Citations** for information in MLA style:

Meidob Volcanic Field, Wikipedia, No author web, 24, November 2009

[]

Google Earth

Waw an namous - AA

 * World Map** (insert world map here) with citation (google earth )
 * World Map** (insert world map here) with citation (google earth )
 * World Map** (insert world map here) with citation (google earth )
 * World Map** (insert world map here) with citation (google earth )
 * Volcano Data**
 * Volcano Name: || Waw an namous ||
 * Location: || Middle of sahara desert ||
 * Tectonic Plate: || Unknown ||
 * Height: || 547 m ||
 * Type of Volcano: || Scoria ||
 * Rock type of lava: ||  ||
 * Setting: || Dessert ||
 * Date of Last Eruption: || Unknown ||
 * Type of Last Eruption: || Unknown ||
 * Detailed map** etailed map here) with citation (google maps )

· **Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL) The typical erupton for my volcano wold be devastating. The magma in my volcano is runny and because of it’s steep sides runs very fast and for a very long time. Hot rocks shoot out of the top of the volcano and can land two of three miles away and huge bolders can role down the slope of the volcano. Gases are released from the top of the volcano causing a smell like rotten eggs the death tole would be in the hundreds. · · []
 * Topographic Map** (insert topographic map here) with citation (URL)

The lava would travel very fast because of the volcano’s steep sides so any viliges close by would not have a lot of time to evaquate. The lava is very runny so it adds to the danger and quickness of the lava. In past eruptons the volcano has shot rocks and thay have landed miles away. If one of thease rocks had landed on a person they would be killed instantly and the rocks were so hot that if they hit a building the building would catch on fire. Viliges would be buried in two to three feet of molten lava. Bolders would role down the side of the volcano crushing people and houses. The erouption would be devastating to any people who lived within a two mile radeas of the volcano hundreds of people would die. But lucky for us it is extinct and in the middle of the saraha dessert. No hazards for my volcano it has been extinct for thouseds of years
 * Hazards:** (type your description below)
 * Citations** for information in MLA style: []

Fogo - HM

 * World Map ** (insert world map here) with citation (URL)[[image:HMWorld_map.jpg]]
 * World Map ** (insert world map here) with citation (URL)[[image:HMWorld_map.jpg]]
 * World Map ** (insert world map here) with citation (URL)[[image:HMWorld_map.jpg]]
 * World Map ** (insert world map here) with citation (URL)[[image:HMWorld_map.jpg]]

The Typical Eruption for Fogo the volcano is when the lave flows out the sides most of
 * Volcano Data**
 * Volcano Name: || Fogo ||
 * Location: || Off the coast of Africa ||
 * Tectonic Plate: || No tectonic plate. ||
 * Height: || 9,279 feet (2,829 m) ||
 * Type of Volcano: || Stratovolcano ||
 * Rock type of lava: || ||
 * Setting: || Hot spot off the coast of Africa. ||
 * Date of Last Eruption: || 1995 ||
 * Type of Last Eruption: || ||
 * Detailed map ** (insert detailed map here) with citation (URL)[[image:HMDetailed_map.jpg]]
 * Typical Eruption: ** (type your description below) – you may include an eruption map with citation (URL)

the time. Its an exploding volcano which means that it doesn’t just dribble out the top it

litteraly blows its top. In addition to that a huge cloud of ash was blown into the sky.

Every time fogo erupts it has earthquakes before it actulay erupts. Six days before. During the eruption the volcano makes lava bombs. Every 3-8 seconds there was a very

loud mini explosion of gas. Along with the explosions some parts of the cone may fall

off. Fogo has historic-aged lava that goes into the water around it.

So to some up a little First there is some earth quakes before the actual erution. Then

theres the erution witch will nomally blow its top. Remember it doesn’t just dribble it

blows right up. Along with the ginormous cloud of ash that was relased into the sky.

And don’t for get about the lava bombs. And of course the caving-in cone.

HYPERLINK [] " INCLUDEPICTURE "http://volcano.si.edu/volcanoes/region18/capeverd/fogo/18fog01s.png " \* MERGEFORMATINET It’s a hot spot. So Theres a bunch of volcanos everywhere all next to each other. There
 * Topographic Map ** (insert topographic map here) with citation (URL) http://volcano.si.edu/world/volcano.cfm?vnum=1804-01=&volpage=var
 * Hazards:** (type your description below)

was a lot of ash in the air. Sufficating all kinds of people and probably animals. The

Earth quakes are also a big hazard that effects everybody around them. And theVolcano I

guess has some effect in the hazards of harming people.

HYPERLINK "http://volcano.si.edu/world/volcano.cfm?vnum=1804-01=&volpage=var" __ http://volcano.si.edu/world/volcano.cfm?vnum=1804-01=&volpage=var __.
 * Citations ** for information in MLA style: HYPERLINK "http://hvo.wr.usgs.gov/volcanowatch/1995/95_04_21.html" __ http://hvo.wr.usgs.gov/volcanowatch/1995/95_04_21.html __.

HYPERLINK "http://volcano.si.edu/volcanoes/region18/capeverd/fogo/18fog01f.png" INCLUDEPICTURE "http://volcano.si.edu/volcanoes/region18/capeverd/fogo/18fog01s.png" \* MERGEFORMATINET

Volcano Project

Visoke - AuL

 * World Map ** :
 * World Map ** :
 * World Map ** :
 * World Map ** :
 * Volcano Data **
 * Volcano Name: || Visoke ||
 * Location: || DRC/Rwanda ||
 * Tectonic Plate: || African Plate ||
 * Height: || 3711 meters. ||
 * Type of Volcano: || Strato Cone. ||
 * Rock type of lava: || Andestic. ||
 * Setting: || Democratic Republic of Congo/Rwanda Border ||
 * Date of Last Eruption: || In 1957. ||
 * Type of Last Eruption: || Created a Mugogo volcano. ||

**
 * Detailed Map:


 * Typical Eruption: ** My volcano is a Strato/Composite, it is a explosive eruption. It is set on a convergent plate, which is the African plate. It is not near an Ocean, a tsunami is not a hazard. The shape is steep and large, and is made of alternating layers of tephra and lava. The explosive eruptions are due to andesitic magma, which is high in gas and silica. Some eruptions are minor+flow easily (thin lava with less silica) and other eruptions are explosive (viscous lava with more silica.)
 * Hazards: ** Made of both thin and thick lava. Some eruptions are minor and flow easily (thin lava with less silica.) Other eruptions are explosive (viscous lava with more silica.)You don’t know when it is going to be a minor eruption or explosive eruption. It is on a convergent plate which is the African plate. A tsunami is not a hazard because it is not close enough to the ocean. The population is very rural, not many people at all. People are not a hazard.
 * Citations ** : [] (topographical map)

[] (Information all on this site)

Jebel Marra - CB

 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * Volcano Data**
 * Volcano Name: || Jebel Marra ||
 * Location: || [|12°57′00″N]  [|24°16′12″E]  ||
 * Tectonic Plate: || African Plate ||
 * Height: || 3,042 m (9,980 ft.) ||
 * Type of Volcano: || Shield Volcano ||
 * Rock type of lava: || High Silica Magma ||
 * Setting: || Range of Moutains, Volcanic Field ||
 * Date of Last Eruption: || 2,000 BC ||
 * Type of Last Eruption: || BOOM ||


 * Detailed map** (insert detailed map here) with citation (URL)
 * Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL)


 * N/A**

Since the last eruption was in 2000 BC, there is no record that can accurately tell us what the hazard is.
 * Topographic Map** (insert topographic map here) with citation (URL)
 * Hazards:** (type your description below)


 * Citations** for information in MLA style:

//EarthTools - Find places, latitude/longitude, sunrise/sunset, elevation, local time and time zones//. Web. 30 Nov. 2009. .

"Marrah Mountains -." //Wikipedia, the free encyclopedia//. Web. 30 Nov. 2009. .

Cumbre Vieja La Pamlma - SCG
A Typical eruption is a basaltic eruption! A basaltic eruption is an eruption that is made up of ash and rocks. This is usually hotter then the other types of magma. This is also made/ know by the ocean crust. One of the Hazards that I thing is that when or if the volcano erupts and heads towards the ocean.
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * World Map** (insert world map here) with citation (URL)
 * Volcano Data**
 * Volcano Name: || Cumbre Vieja La Pamlma ||
 * Location: || Canary Islands ||
 * Tectonic Plate: || African Plate ||
 * Height: || 1310m ||
 * Type of Volcano: || Strato volcano ||
 * Rock type of lava: || Basaltic ||
 * Setting: || Hot spot ||
 * Date of Last Eruption: || 1971 ||
 * Type of Last Eruption: || Basaltic ||
 * Detailed map** (insert detailed map here) with citation (URL)[[image:file:///C:/DOCUME%7E1/SAMANT%7E2/LOCALS%7E1/Temp/msohtml1/01/clip_image004.jpg width="575" height="387"]]
 * Typical Eruption:** (type your description below) – you may include an eruption map with citation (URL)
 * Topographic Map** (insert topographic map here) with citation (URL) [[image:file:///C:/DOCUME%7E1/SAMANT%7E2/LOCALS%7E1/Temp/msohtml1/01/clip_image006.jpg width="474" height="411"]][[image:SCGtopo.GIF]]
 * Hazards:** (type your description below)


 * Citations** for information in MLA style:

[|http://www.tulane.edu/~sanelson/geol204/volcan&magma.htm], Date: 11/ 23/ 09 [], Date: 11/ 23/ 09 Google Earth, Date 11/ 13/ 09 to 11/ 23/ 09