The elevation of the base of a landform above sea level can vary significantly depending on the specific landform in question. For example, the base of a mountain might be several hundred to several thousand meters above sea level, while a valley or plain could be at or near sea level. To provide an accurate answer, I would need more specific information about the landform in question.
it has 5faces and 8edges,5vertices and 4 corner
A square pyramid has 5 * * * * * The above answer has nothing to do with the question. A triangular pyramid has 6 edges. Three edges form the triangular base. Another 3 edges rise from the three vertices of the triangular base to the apex of the pyramid. 3 + 3 = 6. OK?
No. Polyhedra are three-dimensional objects, and the base of any prism, strictly speaking, should be two-dimensional. Any convex polygon (which is two-dimensional) can form the base of a pyramid. A circle, which is technically not a polygon, is the only convex two-dimensional figure that cannot form the base of a pyramid because it forms the base of a cone.
Nine, if the prism has both a base and a top (plus the seven sides). Nine faces is customary for a heptagonal prism (but there are variants ... see below). If the prism is shaped in the form of a pyramid, then eight. There are seven faces, above the plane, plus its base, making eight total faces. (Hepta- is the Greek root word for the number seven.)
It is not possible to answer the question because.No units are given.It is not clear what aspects of the base is 6: its side length, area, perimeter, diagonal ...It is not clear what has an area of 8.It is not clear whether the height refers to the vertical height or slant height.I suggest you reconsider the question and resubmit it in a form that provides the above information.
Most clouds form between 1,000 to 7,000 meters (3,000 to 23,000 feet) above ground level. This range varies depending on the type of cloud and weather conditions.
meters
Low clouds typically form at altitudes below 6,500 feet (2,000 meters) above ground level. The upper height range for low clouds is typically around 6,500 to 20,000 feet (2,000 to 6,000 meters) above ground level.
cirrus
The height of a landform in relation to sea level is called its elevation. The elevation is typically measured in feet or meters above sea level and is an important factor in determining the topography and climate of a region.
Clouds are mainly classified by their appearance, altitude, and the processes that form them. They are categorized into three primary types based on height: low-level clouds (up to 2,000 meters), mid-level clouds (2,000 to 6,000 meters), and high-level clouds (above 6,000 meters). Additionally, clouds can be further classified by their shape, such as cumulus, stratus, and cirrus, which indicate different weather conditions and atmospheric processes.
Mammatus clouds typically form at altitudes ranging from 6,500 to 25,000 feet (about 2,000 to 7,600 meters) above sea level. They are often associated with severe thunderstorms and can appear as pouch-like structures hanging underneath the base of a cloud. The exact height can vary based on atmospheric conditions and the type of clouds from which they develop.
Mount Everest stands at 29,032 feet (8,848 meters) above sea level, which means it typically rises well above cloud level. Clouds generally form at lower altitudes, so Everest often stands high above them on clear days.
When a dome forms high above sea level
Cirrus clouds form above 6000 meters, while stratus clouds typically form at lower altitudes. Cirrus clouds are thin and wispy, often seen at high altitudes, while stratus clouds are usually lower in the sky and appear more spread out in a layered formation.
Cirrus clouds form above 6000 meters. They are thin, wispy clouds that are composed of ice crystals and indicate fair weather or the approach of a warm front. Stratus clouds are typically lower in altitude and are more uniform in appearance compared to cirrus clouds.
They can form 30,000 feet above the surface or right above the ground. It just depends when rising air cools to its dew point, whereupon condensation will occur. This is called the lifting condensation level.