Mountains

Olympus Mons is a large shield volcano on Mars, and it is the tallest volcano in our solar system. It was formed through volcanic activity rather than an explosion. The volcanic activity on Mars is different from explosive eruptions seen on Earth.

So far we have not been able to see any surface features on Saturn, due to the heavy and constant cloud layer. This means we don't even know if there are any mountains on Saturn, let alone the height of them. Scientists are continuing to study this planet. The Cassiniâ??Huygens space probe is there now and will remain until at least 2017, making observations and collecting data.

Peak absorbance refers to the wavelength at which a substance absorbs light most strongly. It is commonly used in spectrophotometry to determine the concentration of a substance in a solution by measuring the absorbance at its peak wavelength.

Mount Ararat and Mount Everest are not connected geographically. Mount Ararat is located in Turkey, while Mount Everest is in Nepal. They are two separate and distinct mountains with no physical connection between them.

The highest peaks of the Hawaiian mountains, like Mauna Kea on the Big Island, can receive snow during the winter months. However, the amount of snowfall varies from year to year and is typically light compared to snowfall in more northern regions. Snowfall is most common between December and February.

The height of Mt. Pissis is approximately 6,793 meters (22,287 feet) above sea level, making it the second highest peak in the Western Hemisphere.

Yes, a mountain can become a volcano if tectonic activity causes magma to rise and erupt through the surface. On the other hand, a volcano can also become a dormant or extinct mountain over time if there is no longer any active magma movement.

mount pelee measures 4,582FT (1,397 M)

A single dime has a thickness of 1.5 mm. A million stacked dimes would reach 1,350,000 mm (1.35 km), or just a smidge over 4,429 ft.

Denali, also known as Mount McKinley, is host to a variety of plant life due to its vast elevation range. At lower elevations, you may find spruce and birch forests, while higher up, alpine plants like saxifrage, lichens, and mosses thrive. Above the treeline, only hardy plants like dwarf willows and alpine azaleas can survive in the harsh conditions.

Sunspots are dark because they are cooler than the surrounding area on the Sun's surface, known as the photosphere. The magnetic fields near sunspots inhibit the flow of hot gases from below, causing them to be cooler and appear darker in comparison.

Mount Nyiragongo erupted on the 21 January 2002 in the Democratic republic of Congo.

The peak of Mount Kilimanjaro is located in Tanzania, East Africa. It is the highest mountain on the African continent, standing at approximately 19,341 feet (5,895 meters) above sea level.

Atmospheric pressure decreases as you go from the top of a mountain to sea level. This is because there is less air above you at higher altitudes, leading to lower pressure. Conversely, at sea level, more air is pressing down from above, resulting in higher atmospheric pressure.

Mount Wilhelm in Papua New Guinea stands at 4,509 meters (14,793 feet) tall, making it the highest mountain in the country.

Breathing is more difficult at high altitudes because the air is thinner, which means there is less oxygen available per breath. This can lead to altitude sickness in some individuals, as the body needs time to acclimate to the lower oxygen levels. The reduced air pressure at higher altitudes can also make it harder for the lungs to expand and take in an adequate amount of oxygen.

Clouds form over mountains when moist air is forced upwards by the terrain. As the air rises, it cools and reaches its dew point, causing water vapor to condense and form clouds. The higher elevation of the mountains also contributes to the cooler temperatures required for cloud formation.

Mountains are beautiful and can reach wonderful height. Mount Lhotse II is located in Nepal, and is 26,723 feet tall.

The mountains are cooler because the earth absorbs an amount of sun's heat.
Plus in the group of layers which are called the ionosphere, the sun's heat is absorbed as only the light gases or heated gases are present in that area. Therefore the temperature in the ionosphere reaches 1650 degrees centigrades in the 240 km area (the ionosphere goes on till above 600km).

As we lower down towards earth the temperature decreases, and as the access heat is sent by earth the coolest place is the meeting of stratosphere and troposphere at the height of 11000 meters (11kms) approximately.

So, actually the areas near to the sun do get hot, but till the time it reaches the mountains it gets cooler, and even earth absorbs heat due to which the mountains get cooler.

The pattern of heat is like this:
keys- H-hot, C-cold
H
C
H

The cool air from the ocean is forced up the mountain slopes, where it cools and condenses to form fog. This process, known as orographic lifting, occurs because the air on the ocean side of the mountain is moister and cooler than the air on the other side. As a result, coastal sides of mountains often experience foggy conditions.

The smallest peak in the world is Rysy, which is located on the border between Poland and Slovakia in the Tatra Mountains. It stands at an elevation of 8,199 feet (2,499 meters).

Mt. Shasta is located in the Cascade Range in northern California.

No, mountains are not hollow. They are composed of solid rock and earth materials, typically formed through tectonic processes like plate movements, volcanic activity, or erosion. While some mountains may have small caves or tunnels within them, they are not hollow throughout.

the resting deadly volcano erupted at 8:32 AM