Volcanoes and Earthquakes are two of the most destructive natural disaters. They are the cause of a lot of deaths. They have many interesting facts. Scientests discover the life of these horrible yet, interesting disasters.

Earthquakes

Earthquakes are one of the most powerful disasters on Earth. An earthquake is the shaking of the ground, caused by the shaking of the plates. An earthquake depends on how far the plates move. Millions pf earthquakes happen every year, but only ten can be felt.In Chile on the richter scale it was 9.5 and five thousand people died. The richter scale is named after Charles Richter. Earthquakes happen all the time even if we can't feel them. California is the state that has the most earthquakes happen there in the U.S.A. Some earthquakes happen on land, but most happen on water.

The largest earthquake ever recorded had the magnitude of 9.5 in 1960. No one knows when earthquakes started happening.An earthquake shakes because of valcano action. "Earthquakes are an awesome thing, one we can't control. They're exciting and scary. Even if we could prodect them we couldn't stop them." Earthquakes happen when plates move. The size of the earthquake depends on how much pressure is built up. The Righter scale weighs from 1-10. An 8.5 can change the couse of a river. Rats are sometimes used to find survivers of earthquakes.

Seismic waves create earthquakes. Nobody can really tell when an earthquake is going to happen. After some earthquakes, some resources are hard to find. Earthquakes can create mudslides and tsunamis. Along borders of places eathquakes are often. The border of North America has very large earthquakes especially along the coast of Alaska. Earthquakes can be very noticible or barely felt.

Year
Location
Deaths
Richter Magnitude
1906
San Francisco
700
7.9
1908
Messina, Italy
100,000
7.5
1915
Central Italy
30,000
7+
1920
Gansu Prov., China
150,000
8.6
1923
Tokyo, Japan
200,000
8.3
1932
Gansu Prov., China
70,000
8+
1934
Bihar, India
6,000
8.4
1939
Central Chile
30,000
8+
1939
Anatolia, Turkey
45,000
6.0
1950
Assam, India
2,000
8.4
1960
Agadir, Morrocco
12,000
5.9
1960
Southern Chile
5,700
9.5
1962
Iran
12,000
7.3
1964
Anchorage, Alaska
131
9.2
1968
Iran
18,000
7.8
1970
Chimbote, Peru
50,000
7+
1970
Yunnan Prov., China
10,000
7.7
1972
Managua, Nicaragua
10,000
6.2
1976
Tangshan, China
600,000
7.6
1978
Central Chile
25,000
7.7
1985
Mexico City
175
8.1
1985
Ecuador
7,000
7.3
1987
Armenia
4,000
6.9
1988
San Francisco
25,000
7.1
1990
Iran
61
7.7
1990
Luzon Is., Philippines
35,000
7.7
Volcanoes

A volcano is a mountain or hill made of lava, which comes from deep beneath the Earth's surface. When a volcano erupts, lava and ash build up to make a cone. Some volcanoes give off clouds of ash and gas when they erupt. Others have streams of red-hot lava pouring down their sides. Volcanoes can form on land or on the ocean floor. Some undersea volcanoes grow high enough to reach above sea level and become islands.

Strato volcanoes are tall and are built up by layers of ash and lava from previous eruptions. Because it is lighter than solid rock, magma has been rising to form a huge pool called magma chamber, beneath the volcano. The volcao will erupt when gas is held within the magma bursts out explosively, now that they are under less pressure than when the magma deeper within the Earth.

The explosive escape of the gases from the magma causes a terrible eruption which literally "blows the top" off of the volcano. Gas, blobs of magma, (now called lava), chunks of rock, and fine debris called volcanic ash are blasted upwards. (The ash, because it is very light, may reach heights of sufficient levels to endanger jet airplanes.)

Ash, lava, and rock is ejected out of the volcano. That's why it is called "ejecta". Magma (also called lava) can build up or stretch across land to make a bigger volcano. Mauna Loa in Hawaii is the biggest volcano in North America because it stretches across land, not because it is tall.

 

TYPES OF VOLCANOES

TYPE OF VOLCANO
SHAPE
COMPOSITION
ERUPTION TYPE
Cinder Cone
Straight sides with steep slopes; large summit crater
Basalt tephra; occasionally andesitic
Strombolian
Sheild Volcano
Very gentle slopes convex upward
Basalt lava flows
Hawaiian
Composite
Gentle lower slopes,but sleep upper slopes. concave upward;small summit crater
Highly variable;alternating basaltic to rhyoltic lavas.
Tephra

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About the Authors

Lauren, Madeline, Linsey, and Christine are the makers of this website. We worked hard to find facts and put together the backrounds and games on this site. Lauren and Madeline found facts on volcanoes and some earthquake references. Linsey and Christine did earthquakes. We all work together to make this webpage. Our teacher Ms. Buras helped us with alot of anchoring, backgrounds, and the "Fireworks" parts.

 

References

"Earthquakes." Facts For Learning. Facts For Learning. 03 Feb. 2005 <http://factsforlearning.2facts.com/e-home.asp>.
"Earthquakes." Earthquakes. World Book Online. 04 Feb. 2005 <http://www.worldbookonline.com/wb/Home>.
"Earthquakes." Earthquakes. Google. 04 Feb. 2005 <http://www.google.com/>.
"Earthquakes." Earthquakes. Yahooligans. 04 Feb. 2005 <http://yahooligans.yahoo.com/>.