For the past several days, we have been making our way over an underwater mountain chain called the Mid-Atlantic Ridge, or MAR for short. This ridge, which snakes its way southward from Iceland through the North and South Atlantic, results from the spreading of two tectonic plates and the bubbling up of molten rock to form new sea floor. Of course this is happening at a snail’s pace—the two plates are separating at a rate of only 2.5 centimeters per year on average. Read More→