Answer:
time
Explanation:
weather is the atmospheric condition of a place over a short period of time, while climate is the weather condition prevailing in an area over a long period of time. From the two definitions above we can see that weather is the condition over a short period of time while climate is over longer periods, therefore the primary difference between them is time.
Answer:
The distance between the two slits is 40.11 μm.
Explanation:
Given that,
Frequency ![f= 6.37\times10^{14}\ Hz](https://tex.z-dn.net/?f=f%3D%206.37%5Ctimes10%5E%7B14%7D%5C%20Hz)
Distance of the screen l = 88.0 cm
Position of the third order y =3.10 cm
We need to calculate the wavelength
Using formula of wavelength
![\lambda=\dfrac{c}{f}](https://tex.z-dn.net/?f=%5Clambda%3D%5Cdfrac%7Bc%7D%7Bf%7D)
where, c = speed of light
f = frequency
Put the value into the formula
![\lambda=\dfrac{3\times10^{8}}{6.37\times10^{14}}](https://tex.z-dn.net/?f=%5Clambda%3D%5Cdfrac%7B3%5Ctimes10%5E%7B8%7D%7D%7B6.37%5Ctimes10%5E%7B14%7D%7D)
![\lambda=471\ nm](https://tex.z-dn.net/?f=%5Clambda%3D471%5C%20nm)
We need to calculate the distance between the two slits
![m\times \lambda=d\sin\theta](https://tex.z-dn.net/?f=m%5Ctimes%20%5Clambda%3Dd%5Csin%5Ctheta)
![d =\dfrac{m\times\lambda}{\sin\theta}](https://tex.z-dn.net/?f=d%20%3D%5Cdfrac%7Bm%5Ctimes%5Clambda%7D%7B%5Csin%5Ctheta%7D)
Where, m = number of fringe
d = distance between the two slits
Here, ![\sin\theta =\dfrac{y}{l}](https://tex.z-dn.net/?f=%5Csin%5Ctheta%20%3D%5Cdfrac%7By%7D%7Bl%7D)
Put the value into the formula
![d=\dfrac{3\times471\times10^{-9}\times88.0\times10^{-2}}{3.10\times10^{-2}}](https://tex.z-dn.net/?f=d%3D%5Cdfrac%7B3%5Ctimes471%5Ctimes10%5E%7B-9%7D%5Ctimes88.0%5Ctimes10%5E%7B-2%7D%7D%7B3.10%5Ctimes10%5E%7B-2%7D%7D)
![d=40.11\times10^{-6}\ m](https://tex.z-dn.net/?f=d%3D40.11%5Ctimes10%5E%7B-6%7D%5C%20m)
![d = 40.11\ \mu m](https://tex.z-dn.net/?f=d%20%3D%2040.11%5C%20%5Cmu%20m)
Hence, The distance between the two slits is 40.11 μm.
They are falling under the sole influence of gravity all objects<span> will </span>fall<span> with the </span>same<span> rate of </span><span>acceleration needless of there size</span>
Answer:
Sea-floor spreading occurs in the oceanic ridges. In there, volcanic activity, together with the gradual movement of the bottom, form new oceanic crust. This allows a better understanding of the continental drift explained by the theory of plate tectonics.
The greatest evidence for Sea-floor spreading is the oceanic trenches, the oceanic ridges, the magma protruding to the surface and the new seafloor.
In previous theories, continents were assumed to be transported across the sea. Harry Hess, in the 1960s, proposed the idea that the seabed itself moves as it expands from a central point. The theory is now accepted, and the phenomenon is thought to be caused by convection currents in the upper layer of the mantle.