On the Earth's surface, the depth is between 8-64 kilometers.
4 million approx, 40 killometres = 40,000 metres x 100 = 4 million centimetres
Soil temperature can vary based on location, depth, and time of year. It is typically measured at a depth of 4 inches (10 cm) below the surface. For most plants, the ideal soil temperature ranges between 60-75°F (15-24°C) for optimal growth and root development.
No, the density of Earth's crust varies depending on the type of rock and location. Generally, continental crust is less dense than oceanic crust. Continental crust is composed mostly of granite and has an average density of about 2.7 g/cm^3, while oceanic crust, which is mainly basalt, has an average density of about 3.0 g/cm^3.
Assuming a basketball has a diameter of around 24 cm (0.24 m), and the earth's surface area is roughly 510 trillion square meters, a mole of basketballs (6.022 x 10^23 basketballs) would cover the earth to a depth of approximately 1.2 meters.
The density of Earth's mantle varies depending on its depth. The part right below the crust has a density of about 3.4 grams per cubic centimeter while the lowest part of the mantle is 5.6 grams per cubic centimeter.
A line has no width nor depth, so it has no surface, thus its surface area is 0 cm2
suface area: 378cm2 Volume: 882cm3
4 million approx, 40 killometres = 40,000 metres x 100 = 4 million centimetres
3 cm if you times divide by a number 1 3rd of it depth in cm.
No, the crust and mantle do not have the same density. The Earth's crust is less dense, primarily composed of lighter silicate minerals, while the mantle is denser due to its composition of heavier silicate and magnesium-rich minerals. Typically, the continental crust has a density of about 2.7 g/cm³, whereas the mantle density ranges from about 3.3 to 5.7 g/cm³, depending on depth and composition.
20-30 Cm below the surface of the pool water.
Soil temperature can vary based on location, depth, and time of year. It is typically measured at a depth of 4 inches (10 cm) below the surface. For most plants, the ideal soil temperature ranges between 60-75°F (15-24°C) for optimal growth and root development.
It has volume √187200 cm³ which is approx 432.7 cu cmIt has dimensions: √(276 12/13) cm by √(36 1/9) cm by √(18 18/25) cmwhich is approx: 16.6 cm by 6 cm by 4.3 cm--------------------------------------------------------------------How this is solved:It has the dimensions of a cuboid are length, width and depth.Thus the three adjacent faces are given by:length × width = 100 cm²width × depth = 72 cm²depth × length = 26 cm²Multiplying all three equations together gives:(length × width) × (width × depth) × (depth × length) = 100 cm² × 72 cm² × 26 cm²→ length² × width² × depth² = 187200 cm^6→ (length × width × depth)² = (187200 cm³)²→ length × width × depth = √187200 cm³But for a cuboid:volume = length × width × depth = √187200 cm³ ≈ 432.7 cu cmGoing back to the original three equations above, rearranging (3):3) depth × length = 26 cm²→ depth = 26 cm² ÷ lengthSubstituting in (2):2) width × depth = 72 cm²→ width × (26 cm² ÷ length) = 72 cm²→ width = 72/26 × lengthSubstituting in (1):1) length × width = 100 cm²→ length × (72/26 × length) = 100 cm²→ length² = 2600/72 cm²→ length = √(36 1/9) cm ≈ 6 cmSubstituting in (3):3) depth × length = 26 cm²→ depth × sqrt(36 1/9) cm= 26 cm²→ depth = 26 ÷ sqrt(36 1/9) cm→ depth = √(18 18/25) cm ≈ 4.3 cmSubstituting in (2):2) width × depth = 72 cm²→ width × sqrt(18 18/25) cm = 72 cm²→ width = 72 ÷ sqrt(18 18/25) cm→ width = √(276 12/13) cm ≈ 16.6 cmNote that length, width and depth can be any of the three dimensions; the cuboid has dimensions:√(276 12/13) cm by √(36 1/9) cm by √(18 18/25) cmwhich is approximately:16.6 cm by 6 cm by 4.3 cm
To calculate the volume of water in a pool measuring 244 cm by 66 cm, we need to know the depth of the pool. Assuming a standard depth of, for example, 60 cm, the volume would be calculated as length × width × depth. Using this depth, the volume would be 244 cm × 66 cm × 60 cm = 967,680 cm³. This is equivalent to approximately 967.68 liters of water.
In Kelowna, British Columbia, the frost line typically reaches a depth of about 30 to 36 inches (76 to 91 cm) below the surface. This depth can vary slightly depending on local soil conditions and weather patterns. It's important for construction projects to consider this depth to prevent frost heave and related damage. Always consult local building codes for the most accurate and specific information.
Oceanic crust is denser than continental crust. Oceanic crust has a density of about 3 g/cm^3, while continental crust has a lower density of about 2.7 g/cm^3.
To calculate the surface area of a rectangular prism with dimensions 6 cm, 8 cm, and 10 cm, use the formula: Surface Area = 2(lw + lh + wh), where l is length, w is width, and h is height. Plugging in the values: Surface Area = 2(6 cm * 8 cm + 6 cm * 10 cm + 8 cm * 10 cm) = 2(48 cm² + 60 cm² + 80 cm²) = 2(188 cm²) = 376 cm². Therefore, the surface area is 376 cm².