Given, g = 9.8 m/s2 h = 25 m
u = 0 m/s h = ut + ½at2
25 = 0 + 0.5 x 9.8 x t2
t2 = 50/9.8
t2 = 5.1
t = 2.26 s
The stone will take 2.26 seconds to reach the water.
The depth in the ocean is measured by sounding using echo-sounders. Nowadays satellites are also used for this purpose.
because the upthrust force of the water acting on the stone was pushing the stone upwards meaning it was acting against the downwards weight of the stone (its weight). This meant that the downwards force was decreased and therefore felt lighter :)
Resistance of water is probably defined as pressure being applied by water on objects and as it's stated in fluid mechanics books pressure increases as height decreases or depth increases, so simply the answer is "yes".
The depth of water. One fathom = six feet.
The relation ship between average precipitation and the depth of the soil is the moister and the water vapor water evaporates and one is a solid and the other is a solid.
When a stone is dropped in water, the force of impact pushes the air out of the small crevices and pores in the stone. This trapped air is then released in the form of bubbles as the stone sinks in the water.
If the glass is even partially filled a stone thrown at sufficient speed will splash water below the kinetic energy of the stone will be dissipated by transferring it to the water. However if the stone is gently dropped into the glass of water (and it was full or nearly full) then the stone which is not soluble in water will displace an amount of water equal to its volume which will overflow.
The spike or droplet of water that rises above the surface when a stone is dropped into water is called a "crown splash" or "crown". It occurs due to the displacement of water caused by the sudden impact of the stone.
The sun can't reach the thermocline layer to heat that depth of water
The sun can't reach the thermocline layer to heat that depth of water
The sun can't reach the thermocline layer to heat that depth of water
It stops where sunlight can't reach!
28.224m
For a water well, until you reach the water table. The depth will vary.
The depth to the water table is the distance from the ground surface to the top of the saturated zone. The depth of a well must be drilled below the water table to ensure water can be extracted. The well should be drilled deep enough to reach the water-bearing aquifer but not so deep that it goes below the water table.
The sun can't reach the thermocline layer to heat that depth of water
Depth of water