Since nobody has confirmed these, I guess I will.Giantpants wrote: ↑Fri Sep 13, 2019 11:46 am1. It’s like a flattopped seamount, which formed by erosion of a seamount (formed by volcanism) to have a flat topSciolyMaster wrote: ↑Fri Sep 13, 2019 9:08 am 1. What is a guyot? How does one form?
2. Describe the three stages of atoll formation. Who first proposed this theory?
3. If a deep-water wave with a wavelength of 12 m is moving at a speed of 50 m/s in 2500 m deep water, what is its period?
4. For the wave in question 3, what is the maximum amplitude it can have before it breaks, assuming it remains in deep water?
2. Atolls are formed by
A. Volcanism forming an island
B. Erosion of the island and formation of a fringing reef, and it lowers in elevation
C. Complete submersion and the island is now a lagoon, oh and also formation of a barrier reef
I feel like I had on my old notes that Darwin came up with it lol
3. 2.77 s, I used the formula wavelength = (g*T^2)/2pi, so if I messed up somewhere lmk lol
4. I’m not so sure abt this one, wouldn’t it just break when it touched the bottom, so like, 2500 m?
Worth a shot lol
All look correct except #4. The answer for that one is 0.857 m, or 6/7 meters. The ratio of wave height to wavelength cannot exceed 1:7 without breaking, so max wave height is 12/7 m, and amplitude is half of wave height, so it would be 6/7 m. I'll ask some now:
1. What kind of data is a Nansen bottle used to collect?
2. What new tool has replaced the Nansen bottle for collection purposes?