The problem most people have is learning to deal with a large 3 dimensional block of material with a specific bulk resistivity instead of two or one dimensional resistors.
I cannot do the concept justice in one small list, but this may help you start to wrap your brain around it:
Imagine a long rectangular bar of material with a square cross section
The end to end resistance (with a square of metal on each end as the electrode contact.)
The resistance is proportional to the length of the bar but is inversely proportional to the side of the square.
Now double the linear size of the bar. It gets twice as long but also twice as wide and the overall resistance is cut in half.
Now imagine such a bar 100 miles long but also tens of miles wide or larger. The resistance between two points 100 miles apart on the Earth's surface will be close to zero.
Oops, we assumed a square electrode on each end. We really have a very small rod or plate at each end. That is where all of the measured resistance and voltage drop happens.
We can keep the same two electrodes and double the distance between them and not increase the resistance at all. Because of that we can say that the resistance of the earth itself, above and beyond the local electrode resistance is zero.
I hope that gives you some introduction to what is going on.