Wait a second!
More handpicked essays just for you.
More handpicked essays just for you.
Chapter 13 earth systems volcanoes
Don’t take our word for it - see why 10 million students trust us with their essay needs.
The volcano of Mount Etna has been on this earth for about 500,000 years and is still currently active. This volcano is located on the east side of Sicily, Italy and stands 10,900 feet tall with a base circumference of 93 miles; it also still has a series of eruptions dating back to 2001. Mount Etna is considered a stratovolcano which means it’s built on top of many layers of lava and ash made from previous eruptions. What makes this volcano so unique is that it has many eruption styles ranging from extreme violent ones to regular lava just flowing from the mouth of it. About “25% Sicily 's population lives on Mount Etna 's slopes.” Etna stands tall above Catania which is a city on the island of Sicily. This stratovolcano plays a major influence …show more content…
The most powerful eruption ever recorded was in “1669, when explosions destroyed part of the summit and lava flows from a fissure on the volcano 's flank reached the sea and the town of Catania, more than ten miles away.” This eruption also paved the way for the way the lava flows from it now however; so when the town was destroyed they rebuilt around the flow of the lava to make sure they’ll be safe. In the year 1775 it erupted again but this time producing big lahar’s, which is a destructive mudflow on the slope of the volcano. “An extremely violent eruption in 1852 produced more than 2 billion cubic feet of lava and covered more than three square miles of the volcano 's flanks in lava flows. Etna 's longest eruption began in 1979 and went on for thirteen years; its latest eruption began in March 2007, and is still …show more content…
This specific volcano however holds the record for longest continuous eruptions. “Mount Etna is a series of nested stratovolcanoes with four distinct summit craters. There are two central craters, called Bocca Nuova and Voragine; the Northeast crater; and the newest Southeast crater, which was formed by an eruption in 1978.” The reason why tectonic plates are so important is because they are the reason how most mountains are formed. The African tectonic plate is major for Africa because it stretches across the entire continent straddling the equator as the prime meridian. It also stretches across some oceanic crust which “lies between the continent and various surrounding ocean ridges.” The African plate actually has 6 major other plates connected to it as well, but Mount Etna is located in the North, on the Eurasian
Kohala Volcano is the oldest of five volcanoes in hawaii. Kohala is estimated of 1,000 years old and it emerged above sea level over 500,000 years ago. The most recent eruptions were 120,000 years ago. That was a long time ago! I wonder when it were to ever erupt again! Hopefully it won't erupt soon! Kohala volcano is extinct. Kohala is so old, that it experienced, and recorded a reversal of magnetic field 780,000 years ago. Kohala is a shield volcano cut by multiple gorges. Between 250,000 and 300,000 years ago, a huge avalanche consumed a slice of the volcano’s northeast flank more than 12 miles wide at the shoreline. The debris spilled more than 80 miles out and onto the ocean floor. The lasting effects can still be seen today in the sheer cliff walls of the windward
On May 22, 1915, an explosive eruption at Lassen Peak devastated nearby areas and rained volcanic ash farther 200 miles to the east! This explosion was the most powerful in a series of eruptions from 1914 through 1917. ...
The ejecta from the eruption moved over land and through the air: the ash that fired out of the volcano was blown as far east as Nebraska in a huge, dark cloud of plinian ash. A nuee ardente billowed over the rim of the volcano and spread lava to the south, east and north, forming a volcanic outcrop now called the Bishop Tuff. Today, an expanding resurgent dome in the center of the depression indicates current magmatic activity beneath the caldera, and earthquake swarms in the last 25 years could also be linked to subsurface magma movement. Clearly, the Long Valley caldera is not dormant, so understanding the eruption that formed the caldera and surrounding features is essential to assessing the region's current and, more importantly, possible future activity.
When the plates mash together on a convergent boundary, they can create an earthquake. A place with a convergent boundary is New Zealand. When the plates pull apart, a divergent boundary, they create a hole in the ocean that causes molten lava to rush up and it causes a volcano to form. A place with a divergent boundary is Iceland. With about 130 volcanoes all together, it has the most volcanoes of any country in the world and is on two tectonic plates. Santorini is currently in an area of earth where the African and Eurasian plate meet, and Atlantis disappeared with a rumble that could have come from a volcano or an
Mount Tambora, located on the Island of Sumbawa, Indonesia is classified as a Stratovolcano. Also known as a composite volcano, Tambora is a tall conical volcano (cone like structure) where layers of the walls are built by hardened lava and volcanic ash. The term composite is used to describe the volcano due to the composite layered structure built from sequential outpourings of eruptive materials1. Among the most common types of volcanoes, Tambora also shares its destructive prowess with best-known volcanoes such as Krakota (1883) and Vesuvius (79 A.D). The Island of Sumbawa is located in the middle of the Lesser Sunda Islands chain (a group of islands in the southern Maritime Southeast Asia) and is in the province of West Nusa Tenggara3. A map of Mount Tambora is shown in Figure 1 to provide a better perspective of its location. Interestingly enough, Tambora forms its own peninsula on Sumbawa, known as the Sanggar Peninsula. In April of 1815, after years of dormancy, Mount Tambora erupted with great intensity, approximately 7 on the volcanic explosivity index, which is shown in Figure 2. It has been estimated that the eject volume of Tambora was 160 cubic kilometres, which represents the largest volcanic eruption in recorded history. The death toll has been projected to be at least 71,000 people, of who over 15% were killed directly from the eruption1. The remaining 75% have been thought to succumb to starvation and disease, as the eruptive fallout decimated the agricultural industry in the region. Following the eruption, a volcanic winter ensued. As sun become less abundant due to clouds of ash, crops and livestock perished. Please note that all definitions appearing in the footnotes are either taken from already referenced so...
Volcanoes have always been a mysterious wonder of the world. Volcanoes have shaped the landscape and the very ground that we all live on. People have written stories of their disastrous eruptions, and painted their marvelous shapes on canvas. The essay will outline some of the more famous volcanoes and how they have impacted are history. Mount Vesuvius that destroy the great city of Pompeii, Krakatoa they spewed deadly ash on small village town, and Mount St. Helen, the only volcano in my own country to every erupt during my own time period.
However, this chronological realignment does not mean that the eruption of Santorini had nothing to do with the Minoan collapse. Most obviously, the island of Thera, which the Minoans probably used as a trading centre or stop-off, was totally destroyed. This would have caused huge problems for the Minoan’s trading empire.
Mauna Loa is the largest volcano in the world measuring 2,000 miles². Mauna Loa is 13,677 feet tall, 74 miles long, and 64 wide. On March 24, 1984, at 1:30 in the morning, Mauna Loa began to erupt. This eruption is known as a quiet eruption. The eruption does not cause the volcano to explode or make much of a loud noise. This is due to the basaltic lava and a low amount trapped gases. It just flows a low viscosity lava out of the volcano. When the eruption started, lava started pooling out of the top of Mauna Loa. Within 2-3 hours about 80% of the crater on top of the volcano was submerged in lava. Many worried that the lava would overflow and run to the Mauna Loa Observatory, but the eruption shifted to go northeast rift zone instead. This instead threatened the nearby city of Hilo, populating 40,000 people. The lava headed straight for the town. On the way, the lava reached a generator and left it destroyed. This took out the power for the observatory on the other side of the volcano. This lava that Mauna Loa erupted is a basaltic lava. Basaltic lava silica content is low and only contains 45-55% silica. This makes the magma more liquid and gives it the ability to move quickly. As the lava approaches the vulnerable city of Hilo, many of the people began evacuating. Luckily, the lava stopped at the outskirts of town, burying 16 miles of land owned by the state, never to be seen again. The
Stories about volcanoes are captivating. Myths come in different versions, but all of them are capable of capturing yours, and everybody’s imagination.
Volcanism is a major part of the Galapagos and their formation. The island chain is positioned on the Nazca Plate, which is subducting beneath the South American Plate at a geologically rapid pace of 2.5 inches per year. In addition, this Nazca Plate is located directly on top of the Galapagos Hotspot. It is here that mantle plumes melt Earth’s crust, creating volcanoes as a product. The oldest island was first shaped by this ...
First you might need to know definition of tectonics. It is a theory in geology. The lithosphere of the Earth is divided into a small number of plates which float on and travel independently over the mantle and much of the Earth’s seismic activity occurs at the boundaries of these plates. That is the official definition of Plate tectonics. secondly, this plate covers many parts of continents. plate boundaries don’t go according to Continents boundaries, they make their own boundaries. The North American plat...
Rocks are hard but in time they can bend or fold producing folded mountains. The Alps formed as the Eurasian plate pushed against the African plate. Other examples of folded mountains are the Rockies, Himalayas, Appalayas, and the Andes. Fault-block mountains are formed when one plate pushes or pulls away from another plate. On the Earth, hot currents of magma or molten rock may well up and crack the weakened crust above.
Volcanoes can be one of the most destructive forces on Earth. It is estimated that some
Volcanoes are formed when magma is expelled from the Earth’s surface, resulting in volcanic eruptions consisting of ash and lava. Over time, the lava cools and forms into rock on the Earth’s surface. Whenever an eruption occurs, the newly-formed rock from the lava layers continuously until the volcano takes its shape. Volcanic eruptions have taken place for thousands of years, and even today, according to the U.S Geological Survey (2010), there are approximately 1500 active volcanoes located throughout the world.
Mount Vesuvius is a strato-volcano consisting of a volcanic cone (Gran Cono) that was built within a summit caldera (Mount Somma). The Somma-Vesuvius complex has formed over the last 25,000 years by means of a sequence of eruptions of variable explosiveness, ranging from the quiet lava outpourings that characterized much of the latest activity (for example from 1881 to 1899 and from 1926 to 1930) to the explosive Plinian eruptions, including the one that destroyed Pompeii and killed thousands of people in 79 A.D. At least seven Plinian eruptions have been identified in