Recall from the chapter on Fractal Geography that a coastline – such as that of Britain – shows more and more detail the closer we zoom into it. If we ask “How long is the coast of Britain,” the answer is that it depends on how closely you look at it, or how long your measuring stick is. If you measure the coastline by taking a map and placing a ruler around the edge you can get a certain value for the perimeter. But if you were to walk around the beaches of Britain and add up all your steps, you’d arrive at a very different (and larger) perimeter. But that value is also an approximation. To get a more accurate value, you’d have to measure the length around every boulder, and every rock, every pebble, and even every grain of sand. And at a microscopic level, sand is a fractal as well, and cannot be easily measured. The answer is: the coastline gets longer and longer as you measure it more closely, and it approaches infinity. This is why the fractal dimension is a very useful concept to describe a coastline. Source: Fractal Foundation Online Course
Well. A coastline approaches infinity, does it? That helps to explain why coastal roads are the same wherever you go: slow. The ones in Newfoundland are no exception.
But the views are generally worth the effort and time it took to get to them.