The total depth of the Earth from the surface to its center is approximately 6,371 kilometers (about 3,959 miles). This measurement represents the average radius of the Earth, as the planet is not a perfect sphere but slightly flattened at the poles and bulging at the equator. Consequently, the depth can vary slightly depending on the location, but 6,371 kilometers is widely accepted as the standard figure.
A flat surface is no more that a plain horizontal surface with no depth. For example the surface of a table top is a flat surface, that is the surface only, not the depth of the top or the rest of the table
The area of a circular surface uses the formula pi*the radius squared. So for your question the radius is half the diameter or 4 feet Pi is basically 3.14 3.14*4*4=50.24 square feet. The depth of the water does not apply But if your looking for the volumn you multiply the area*depth or 50.24*1.5 = 75.36 cu.ft. To calculate the number of gallons multiply volumn*7.48 = 563.73 gal.
The depth of a lake at a center point is a function of the distance of that point from shore.
Volume= surface area (length x width) x depth re arrange to surface area= depth= Volume/Area Area= Volume/Depth
A flat surface with an infinite length and width but no depth is called a plane.
its hot and the deeper you go the hotter it gets
Since the earth is not perfectly round, distances vary slightly. From the poles to the center its about 3950 miles. From the equator to the center its about 3960 miles The correct answer is the earth has an equitoral circumference of ~ 24,900 mi and diameter of ~ 7,926mi. With these facts we devise the surface to core distance to be ~3963mi at the equator and 3950mi from the poles.
The force of gravity is proportional to the masses of the two objects and inversely proportional to the square of the distance between them. As a result, a gravity of one fourth that on the surface of the Earth would be observable at an altitude equal to the radius of the Earth, i.e. 6400 km. Note: This is up, in the air, not down, into the Earth. This distance is in outer space.In the other direction, the force of gravity gets smaller as one goes deeper into the earth. This is because the mass outside your current radius (as you descend) does not contribute. The mass inside your current radius is proportional to the cube of the radius. Gravity is proportional to this mass divided by the square of the radius. Therefore, gravity decreases linearly with the radius. So the acceleration of gravity is equal to one fourth its value at the earth's surface at one fourth of the earth's radius, or a depth of approximately 4800 km.
The center of the Earth has not been discovered because it lies at a depth of approximately 6,400 kilometers below the Earth's surface, which is beyond our current technological capabilities to reach.
The average depth of the Earth's surface is approximately 10 kilometers. However, this can vary depending on factors such as topography and geological features.
Pressure and temperature increase with depth beneath the surface of the Earth.
Yes, it is generally hotter underground compared to the Earth's surface. The temperature increases with depth due to geothermal heat from the Earth's core. The increase in temperature is dependent on factors such as location and depth.
The center of the Earth is approximately 6,371 kilometers (3,959 miles) below the surface. This point is known as the Earth's core and consists of a solid inner core and a liquid outer core.
A negligible percentage, significantly less than 1%. Rivers occur only of the surface of the earth, around 70% of which is oceans. Rivers occupy a tine proportion of the remaining surface. Compared to the radius of the earth their depth is negligible so that they occupy a minuscule proportion of the earth's volume.
The radius of the earth is more than 6000km,to reach the centre of the earth we have to dig a whole to this depth which is impossible
The density of Earth materials generally increases with depth below the surface due to the increasing pressure from the overlying layers. As depth increases, the materials experience more compression, leading to higher densities. The variation in density with depth is important for understanding the structure and composition of the Earth's interior.
Absolutely.