Mountains

This is a mixture.

The demand load for 3 ranges rated at 9KW each is 27KW (3 x 9KW) and the demand load for 3 ranges rated at 14KW each is 42KW (3 x 14KW). Therefore, the total demand load for all 6 ranges is 69KW (27KW + 42KW).

Mountains can be formed through plate tectonics, where tectonic plates collide and force the Earth's crust to buckle and rise. They can also be created by volcanic activity, as magma rises to the surface and solidifies, building up over time. Mountains can also form through erosion, as softer rock is worn away, leaving harder rock formations standing tall.

Yes, but only minimally because your weight is gravity's pull on you, gravity weakens the further from the Earth you get.

Here's an equation:

Force = (Gravitational constant x (Earth's mass x Your mass)) ÷ (distance between gravitational centres)²

Gravitational constant gravitational constant = 6.67300 × 10-11 m3 kg-1 s-2

Distance between gravitional centres = distance between your stomach and centre of the earth.

When at 10,000ft(3.117km) above the equator your weight would differ by 1/(6378 squared/(6378 + 3.117)squared) or in simpler terms 0.1%.

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However, at the poles you would weigh slightly less. This is because the Earth is an oblong spheroid, and the radius of the Earth around the poles is 6357km and around the equator 6378km. Therefore there is less mass between you and the centre of the Earth

Therefore if you go from a beach on the Equator to the North Pole you could lose 1 pound and 3 ounces (0.539kg)!

Also the further into the Earth you get the less gravitational pull there is because there is less mass, this means that theoretically if somebody built a hole and you fell down it into the centre of the Earth you would just float!

Transform boundaries cannot form volcanoes.

Mount Everest, located in the Himalayas in Asia, is the highest peak on Earth and is considered the largest fold mountain in the world.

Mount Pinatubo erupts on an irregular basis, about every 3,000 to 5,000 years. The last big eruption began in 1991.It typically will erupt multiple times during an eruption period before going dormant again.

Mount Hood's summit elevation is 11,240 feet (3,426 meters) above sea level. It is a dormant stratovolcano located in the Cascade Range of Oregon, USA.

The elevation of Mount Tambora is around 2,722 meters (8,930 feet) above sea level. It is an active stratovolcano located on the island of Sumbawa in Indonesia.

The buoyant force exerted on a person by the atmosphere decreases as they climb a high mountain due to the lower atmospheric pressure at higher altitudes. This decrease in pressure results in less force being exerted against the person's body.

The Pyrenees Mountains separate France and Spain. The Principality of Andorra, with a population of approximately 84,000, lies in the eastern Pyrenees on this border.

It can also be said to separate Spain and Portugal from the rest of Europe.

According to Wikipedia (refer to the link, below), "The Pacific Ranges [an area encompassing the coasts of Canada and the U.S. States of Washington, Oregon, and California] are part of the southern portion of the Coast Plutonic Complex and has been characterized by rapid rates of uplift over the past 4 million years, which has led to relatively high rates oferosion."

Air pressure decrease with altitude thus the air pressure is the greatest at the mountain base.

Some famous explorers from South Dakota include Meriwether Lewis and William Clark, who led the Lewis and Clark Expedition, and George Armstrong Custer, known for his expeditions in the American West including the Black Hills region of South Dakota.

Complex mountain systems like the Himalayas are the result of tectonic plate collisions, specifically the Indo-Australian plate colliding with the Eurasian plate. The force from the collision causes the Earth's crust to fold and uplift, forming the towering peaks and deep valleys characteristic of mountain ranges.

"The Way to Rainy Mountain" by N. Scott Momaday can be best described as a blend of historical accounts, Kiowa folklore, and personal reflections. It weaves together these elements to create a rich tapestry of the Kiowa people's past and culture. Through lyrical prose and vivid imagery, Momaday captures the essence of his heritage and a sense of connection to his ancestors.

Kennesaw Mountain was formed by geological forces that uplifted and folded the bedrock in the area millions of years ago, creating a prominent peak within the Georgia Piedmont region. The mountain is primarily composed of metamorphic rocks such as schist and gneiss, with some igneous intrusions. Erosion over time has shaped the mountain's current rugged terrain.

Mongolia is a country in Asia with many grassy plains that make good breeding grounds for livestock. Mongolia is also located partially in the Gobi Desert, making it a country with many different climate types.

The three major divisions of the Himalayas from north to south are:

Ø The Great Himalayas/Inner Himalayas/Himadri(Northernmost division).

Ø The Lesser Himalayas/Himachal

Ø The Shiwaliks (Southernmost division).

The earth's crust is made up of several huge plates called techtonic plates. They move, probably energized by heat vectors coming up from the core. When two plates collide, mountains are formed at the colliding edges. Usually one plate is forced down under the other, lifing the other up.

Mount Everest is estimated to have formed around 60 million years ago as a result of tectonic plate movements and the collision of the Indian and Eurasian plates. It continues to rise at a rate of about 4 mm per year due to the ongoing geological processes in the region.

It last erupted in April 13,2009.

The Chagga people are the main ethnic group living around Mount Kilimanjaro in Tanzania. They have a long history of living in the region and are known for their farming practices and unique culture. Additionally, the Maasai people also have a presence in the surrounding area.

The average temperature for mountains can vary greatly depending on the elevation and location. Typically, temperatures tend to decrease by about 3.6°F for every 1,000 feet gained in elevation. Mountainous regions can experience cooler temperatures due to higher altitudes and strong winds. It's common for mountainous areas to have significant temperature variations between day and night.