Mountains

No, to have snow on top (permanently) the height of the mountain must exceed that of the snow line for the particular latitude at which the mountain is located (the snow line is higher at the equator than it is at the poles). Mountains that do not reach this height are not permanently snow capped (they may have snow on in winter months).

There is very little that lives on Mt. Fuji besides a forest and vegetation at the base. The forest is called 'Aokigahara' or 'Sea of Trees' and does have some animals, but largely the forest is uninhabitated. Legend has it that the forest is haunted, but there is little to substantiate this other than stories and rumors. See the realted link for more information on 'Aokigahara'.

The so-called Japanese Alps run the full length of Honshu, the main island of Japan. The ball park estimate for their length is something on the order of 1,000 miles. This "spine" roughly bisects Honshu along its length, and is divided into three moderately distinct regions. From north to south, they are the Hida, the Kiso and the Akaishi Mountains. You might want a link, and you've got one below.

Above sea level, Mt. Everest at 29,028 feet. From base on the seafloor to peak, Mauna Kea at 33,480 feet.
Mount Everest is 8848 meters/29029 feet high.

Mount Krakatau, also known as Krakatoa, is an active volcano located in Indonesia. It measures approximately 813 meters (2,667 feet) in height.

Stone Mountain in Georgia has a relief of approximately 825 feet (251 meters) from its base to its summit. It is known for its massive granite dome that rises prominently from the surrounding landscape.

The difference between a hill and a mountain is that a hill is generally a smaller landform than a mountain. Both are elevated above surrounding areas but hills more often have gently slopping sides, while mountains can have steep sides, even sheer sides. Hills can be the remains of mountains that have been eroded over the ages.

Aconcagua is a mountain located in the Republic of Argentina. Aconcagua is not a volcano, though this is a widespread misconception. This mountain is the highest point in the Andes.

Your mass would not change when climbing a mountain. Mass is a measure of the amount of matter in your body, so it remains constant regardless of your location or elevation. However, your weight might appear to change due to variations in gravitational force at different altitudes.

Colorado

From what I recall, the air at the bottom of a mountain is usually warmer, wetter, and more oxygenated. The air at the top gets less of these three depending on as high up as you go.

Literally, it is a granite monolith...pretty solid inside and lacks an atmosphere. I guess as close as you can get is: Dry, with 0% humidity, and not much wind and pretty much a stable 63 or so degrees depending on how far inside you go. :)

Colonna is an inline Roman typeface based on artwork that was obtained by Stanley Morison in 1926. It was designed as part of a project to increase the range of display faces in Monotype's library. Colonna was originally developed as an advertising face; however, it is at its best when used in large sizes.

Yes, the Cascade Mountain Range is older than the Rocky Mountains. The Cascade Range began forming around 35 million years ago as a result of tectonic activity associated with the subduction of the Juan de Fuca Plate under the North American Plate. In comparison, the Rocky Mountains began forming around 50 million years ago due to the Laramide orogeny.

Well i am pretty sure they are Agniosperms, gymnosperms and ferns i am in year seven and those are the three that our teacher told us about and they usually give you the most common of everything in science so yeah hope that helps bye

John Harte observed that salamander populations were declining in the Rocky Mountains due to climate change. Warmer temperatures were leading to drier habitats, causing disruptions in the salamanders' habitats and reducing their numbers.

A rock mass or mountain peak shaped like a needle is known as a spire or pinnacle. These features are tall, thin, and often have a pointed or jagged top, similar in appearance to a needle. Spire formations are commonly found in mountainous regions and can be formed through erosion or volcanic activity.

A mountain is taller than a hill. A hill must attain a certain height to be considered a mountain. This height requirement varies from culture to culture. There is no standardized height or a world-wide definition for the word "mountain".

its the thing and then it does like yeah thats the answer.

At the summit of Mt. Everest, there are no permanent facilities due to the extreme conditions. Climbers typically spend only a short amount of time at the summit due to low oxygen levels and extreme weather. Summiting Everest requires careful planning, experience, and preparation for a very challenging and dangerous climb.

the altitude of Mt. Everest is 29, 029 ft. above sea level.
The altitude of Mount Everest is 8,848 meters or 29,029 feet high, making it the highest mountain in the world.

Smith Mountain is a man-made reservoir located in Hardy, Virginia, created by damming the Roanoke River. The area around Smith Mountain features rolling hills and forested mountains typical of the Blue Ridge region of Virginia.

Mt. Rainier is an active volcano but is currently not expected to erupt imminently. Volcanic activity is monitored regularly by the United States Geological Survey to provide early warning if any significant changes occur.

Frost shattering is due to temperature fluctuations. During the day when the temperatures are warm, water settles into cracks in rocks. At night the water freezes and causes the cracks to widen. Eventually this causes pieces of rock to shatter from the main rock, this is called frost shattered peaks.

The uplift stage in mountain forming is when tectonic forces push rock layers upward, creating mountains. This can result from the collision of tectonic plates or the movement of hot magma beneath the Earth's crust. As the rock layers are pushed upward, they can fold, fracture, and uplift to form mountain ranges.