At a spreading rate of 2.5 cm/yr, sediments accumulate at 1 cm/kyr. This means that 500 km away from the ridge crest, which is 50,000 cm, sediments would be (50,000 cm / 1 cm/kyr) = 50,000 kyr thick. Therefore, the sediments would be approximately 50,000 cm, or 500 m thick at that distance from the ridge crest.
pebbles are sediments that range in size from 0.2 cm to 6.4 cm.
Sediments of 0.0002 cm in diameter would likely form siltstone, a type of sedimentary rock composed primarily of silt-sized particles. Siltstone has a fine-grained texture, as silt particles are smaller than sand but larger than clay.
To prevent particles of 0.01 cm from settling downstream, a minimum stream velocity of 0.02 m/s is required, based on Stokes' law calculations for settling velocity.
hey....
Given the category and the fact that 'rio' means - river / brook / stream. The answer to your question is that a river does not have a 'height'.
A stream with a velocity of 20 cm/s can transport particles up to fine sand size (0.0625 - 2 mm). Larger particles such as gravel and boulders would require a faster flow velocity to be transported.
Which dimensions are which? For a base of 2 cm, height of 3 cm, and length of 2 cm it would be 5 cm^3. It would be the same if the base were 3 cm, but if the length were 3 cm it would instead be 6 cm^3.
The minimum stream velocity needed to keep a 6.4 cm diameter particle in motion is dependent on factors such as the density of the particle and the fluid, as well as other environmental conditions. However, as a general guideline, the velocity required can be estimated to be around 2-3 cm/s for particles of this size.
It would be about 3.35 cm
Division would be the operation that would convert 15.5m to cm. You would divide by 100.
The minimum stream velocity needed to keep a particle in motion can be estimated using the settling velocity equation. For a 10 cm diameter particle, the approximate minimum stream velocity would need to be around 0.03 m/s to keep it in motion. This value may vary depending on factors such as particle density and fluid properties.