41:12 interesting, but it would have been great having an explanation of how the speed of the spreading creates those different topographies in mid ocean boundaries.
37:10 this is a process that I find unclear. If I follow your diagrams, in step 1 there is upwarping and fault formation. In step 2 there is thinning, but thinning needs to occur due to tensional forces. But if there are faults between the blocks of rock, how can this tensional forces affect the rocks between faults to make them thinner?
![F.HERO Ft. JSPKK x ลำไย ไหทองคำ x M-PEE - ไม่สนิทบิดหมด (Thai Riders Anthem) [Official MV]](http://i.ytimg.com/vi/kPJZ0UihBfk/mqdefault.jpg)
Thanks for posting these videos, my professor did not do this in our class. I very much appreciate it.
41:12 interesting, but it would have been great having an explanation of how the speed of the spreading creates those different topographies in mid ocean boundaries.
37:10 this is a process that I find unclear. If I follow your diagrams, in step 1 there is upwarping and fault formation. In step 2 there is thinning, but thinning needs to occur due to tensional forces. But if there are faults between the blocks of rock, how can this tensional forces affect the rocks between faults to make them thinner?
Guyots