Well, honey, gravity is the culprit here. The strength of gravity on a celestial body determines how tall its mountains can reach before collapsing under their own weight. The higher the gravity, the shorter the peak – simple as that. Keep it real and keep it grounded, just like those mountains should be.
Altitude as a concept was likely first understood by ancient civilizations in relation to the height of mountains or celestial bodies above the Earth's surface. The formal measurement and understanding of altitude in relation to the Earth's elevation above sea level were developed over time through advancements in geodesy and surveying techniques. The term "altitude" itself comes from the Latin word "altitudo," meaning height.
The angular distance from the horizon to the height of a celestial object is known as its altitude. It is measured in degrees, ranging from 0° at the horizon to 90° at the zenith (directly overhead). This measurement helps observers determine how high an object appears in the sky, which is essential for navigation and astronomy.
The Hubble Space Telescope is placed in low Earth orbit at an altitude of about 547 kilometers (340 miles) to avoid atmospheric distortion that hinders image clarity. This height allows Hubble to capture high-resolution images of distant galaxies, stars, and other celestial bodies without the distortion caused by Earth's atmosphere.
Mountains vary in height due to differences in the tectonic processes that form them. Factors like the convergence of tectonic plates, the type of rock layers involved, and the timing of volcanic activity all influence a mountain's height. Additionally, erosion and weathering can also impact a mountain's height over time.
Generally, the youngest mountains are not necessarily the tallest. While younger mountains, formed by tectonic activity, can be quite high, factors such as erosion, geological composition, and the age of the mountain range also play significant roles in determining height. For example, the Himalayas are among the youngest mountains and are also the tallest, but many older mountains, like the Appalachian Mountains, are much lower due to extensive erosion over time.
Trigonometry is used in finding the height of towers and mountains and finding the distance between celestial bodies.
Topography refers to the shape or height of the land. It includes features such as mountains, valleys, and plateaus.
Plateaus and mountains are both elevated landforms that rise above the surrounding terrain, often characterized by steep sides. However, they differ in formation and structure; mountains are typically formed by tectonic forces that create peaks, while plateaus are elevated flatlands that result from volcanic activity, erosion, or sedimentation. In terms of appearance, mountains have a pointed or rugged summit, whereas plateaus have a flat or gently sloping top. Additionally, plateaus tend to cover larger areas horizontally compared to the more concentrated height of mountains.
53''
Height from sea level.
Mountains are classified based on their height and formation, such as volcanic, fold, or block mountains. Valleys are classified based on their shape and formation, such as V-shaped valleys carved by rivers or U-shaped valleys carved by glaciers. Plains are classified based on their elevation, with low-lying coastal plains and high plateaus being common types.
Altitude as a concept was likely first understood by ancient civilizations in relation to the height of mountains or celestial bodies above the Earth's surface. The formal measurement and understanding of altitude in relation to the Earth's elevation above sea level were developed over time through advancements in geodesy and surveying techniques. The term "altitude" itself comes from the Latin word "altitudo," meaning height.
A plateau is a flat elevated landform situated high above sea level in mountainous regions. Plateaus are often characterized by steep sides and a relatively flat top.
The Appalachian Mountains are belived to have been the highest mountains on earth roughfly 466 million years ago. The mountains are divided onto a series of ranges, with the individual mountains averaginf from a height of 3,000 feet (900 m). The highest of the group is Mount Mitchell at a height of 6,684 feet, (2,037 m)
plateaus are very useful because they are rich in mineral deposits. In plateau areas, there may be several waterfalls as several waterfalls as the river falls from great height. The lava plateaus are rich in black soil good for cultivation. many plateaus are great attraction to tourists.
about 1500 mm
1000 ft