Mountains

its 12,098 feet. The above answer is false, ladies and germs. It cannot possibly be correct, because it is 4,730 meteres so if you check your arithmetic, I'm positive you'll find this incorrect. I don't, however, have the correct calculations at this moment, but when I do find them, and I shall, I'll let you all know what the correct answer is. ~Aaron~ Hello there, it's me, Aaron, again. I've found the correct calculations for the height in feet. Mount Trikora is 15,518 feet tall. I dearly hope this helps all of you who are doing homework or are simply bettering your knowledge. Enjoy WikiAnswers! It's helped me alot in my studies! ~Aaron~

Mauna Kea is approximately 13,796 feet (4,205 meters) above sea level, making it the highest point in the state of Hawaii.

Annapurna was formed through the process of plate tectonics, where the Indian Plate collided with the Eurasian Plate, resulting in the uplift of the Himalayas. The intense forces of tectonic activity and the convergence of these plates caused the massive uplift of the Annapurna massif over millions of years.

if something grows a centimeter every year for a million years: the basic formula is a million times a centimeter which is about 1/2 and inch. so the answer would be 5,000,000

You may refer to the following link, which is self explanatory: http://en.wikipedia.org/wiki/Rain_shadow Answered on 26/06/2009 by: Jeril

It depends on where you are measuring from- it is indeed the tallest mountain since its base is on a spot on the floor of the Pacific Ocean. However, Mount Everest is the tallest mountain from sea level.

After a mountain forms, it may undergo erosion through processes like weathering and landslides. Over time, the mountain may decrease in height and size. Additionally, the mountain could become a habitat for various plants and animals as ecosystems develop on its slopes.

yes there are.Infact, scientists have used telescopes to explore venus and there are some mountains there made out of rock that are bigger then 30000 Feet!So that meens bigger then MT.Everest!There are no mountains made out of something else.All the mountains on venus are made out of rock.

Mount Shasta's last known eruption occurred around 1786, based on historical records and studying the geology of the area. The volcano is currently considered to be dormant, with no signs of imminent eruption.

where will i get this stupid answer? really you guys useless idiots

Aconcagua, the highest peak in the Americas, was formed over millions of years through the movement of tectonic plates. It is part of the Andes mountain range, which was created by the collision of the South American Plate with the Nazca Plate. The immense pressure and heat from this collision caused the Earth's crust to uplift and form the towering peak of Aconcagua.

Abraham offered up Isaac on Mount Moriah, as recounted in the Bible in the Book of Genesis.

Rip Van Winkle falls asleep in the mountains after drinking a mysterious liquor given to him by the ghostly figures that he encounters. This liquor causes him to fall into a deep sleep for twenty years.

Mount Teide erupted in 1706 due to the accumulation of pressure from the movement of magma beneath the surface. This pressure eventually led to a volcanic eruption, releasing lava, ash, and gases into the surrounding area.

God created mountains as a part of the natural beauty and diversity of the Earth. They serve important ecological functions by influencing weather patterns, providing habitats for various species, and playing a role in regulating water flow. Additionally, mountains symbolize strength, stability, and majesty in different cultural and religious beliefs.

Mount Whitney was formed as a result of tectonic plate movements along the Sierra Nevada mountain range in California. The rock that makes up the peak is mostly granite, which was pushed up and exposed through erosion over millions of years. The specific geological process that formed Mount Whitney is known as the Sierra Nevada Batholith.

There is no "Mount Novarupta." The volcano known as Novarupta has not yet been able to build up into a mountain. So far it has only managed to create a lava dome that rises 295 feet above the surrounding terrain.

Mt. St. Helens has had several different styles of eruptions through its history. The types of eruptions vary from explosive to dome building.

The explosive history of Mt. St. Helens is relatively well known from the May 18, 1980 eruption that captured world attention at the time. The eruption style was typical of this volcano, pyroclastic flows and lahars were both generated. The flank collapse was more than likely a result of the earthquake under the flank at the time, and is believed to have been the trigger of the eruption itself.

Dome building eruptions have been the most common types of eruptions since the 1980 explosive eruption. There have been several lava domes generated since the summit eruption that generated the crater.

Although they have not been witnessed in historical time, Mt. St. Helens does have a history of passive lava eruptions out of flank vents. This type of eruption although it hasn't been witnessed in a rather long time, it is believed that these types of eruptions have been just as common if not more common than the explosive eruptions we have seen in historical times.

K2, the second-tallest mountain in the world, is 8,611 meters (28,251 ft) above sea level.

Dome mountains form in areas of flat-lying sedimentary rocks that are warped up to create a roughly circular shape. A Utah example is Navajo Mountain, which most likely has a core of igneous rock that arched up the overlying sedimentary rock layers.

To list the mount points on the remote system named bravo that the local system named grape can mount, you can use the showmount command. On the local system grape, run showmount -e bravo to see the exported directories that grape can mount from bravo.

It is difficult to predict exactly when a volcano will erupt. Monitoring by local authorities and scientists is ongoing to detect any signs of increased volcanic activity in Montserrat. It is important to stay informed through official sources in case of any volcanic alerts or warnings.

The last significant eruption of the Soufrière Hills volcano on Montserrat occurred in 2010. Since then, the volcano has remained active with periodic small-scale eruptions and ongoing volcanic activity.