The correct answer is visible light.
Hope this helps.
False its an unbroken loop that allows electrons to flow through constantly
D -
You basically keep varying the coefficient so until the number of atoms for each element is equal. I started with iron to show how you might have to change coefficients but it would be more efficient and quicker to start with oxygen since it changes the value or iron required.
Answer:
D = 230.2 Km
Explanation:
let distance between seismograph and focus of quake is D
From time distance formula we can calculate the time taken by the S wave

From time distance formula we can calculate the time taken by the P wave

It is given in equation both waves are seperated from each other by 17.8 sec
so we have
sec
Putting both time value to get distance value

D = 230.2 Km
Elementary charge used to determine charges of other objects is equal to a charge of electron or proton. It's value is roughly

. All other charges are whole-number multipliers of this elementary charge, meaning that we multiply elementary charge by {...,-2,-1,0,1,2,...}.
To find out if the measured charge can be accepted we need to divide it with elementary charge to see if we get whole number as result.
There are three possible values of measured charge:


As we can see none of the possible values of a measured charge is whole-number multiplier of elementary charge so the researcher should not accept the value.
This charge can be achieved by using quarks which have value of 1/3 of elementary charge but they do not remain stable for long enough.