The shape of Mount Everest is influenced by several geological and climatic factors. Tectonic activity, particularly the collision of the Indian and Eurasian plates, has caused uplift and deformation, shaping its height and contours. Erosion from glaciers, ice, and weathering also plays a crucial role in sculpting its features over time. Additionally, factors such as climate change can affect glacial melt and accumulation, further impacting its shape and structure.
there is no factors
A cone shape.
By the wind
Biotic factors in mountain biomes include plants, animals, and microorganisms. Abiotic factors include temperature, altitude, precipitation, soil composition, and sunlight levels. These factors together shape the unique ecosystems found in mountain biomes.
Locamotion, cell movement, biosynthesis
Factors that affect the shape of leaves include genetics, environmental conditions such as light availability, temperature, humidity, and soil nutrients. Additionally, leaf shape can be influenced by evolutionary adaptations to specific ecological niches and interactions with herbivores or pathogens.
shape, size, and speed
Mount Everest, the tallest mountain in the world, formed due to the collision of the Indian and Eurasian tectonic plates. This collision caused the Earth's crust to fold and uplift, creating the massive Himalayan mountain range. Over millions of years, the forces of erosion and weathering have continued to shape and sculpt Mount Everest into its current majestic form.
shape, size, and speed
It is Slope , Volume of flows , and Streamed Shape.
The Ngong Hills (Kenya) The Cheviot Hills (England)
The shape of an object does not affect its velocity because velocity is determined solely by the object's speed and direction of motion. The shape of an object may affect other factors such as air resistance or aerodynamics, which can influence how quickly the object slows down or changes direction, but it does not directly affect its velocity.