WEBVTT 1 00:00:03.400 --> 00:00:05.400 So that's kind of what it looks like, that's 2 00:00:05.400 --> 00:00:07.400 the detail that we get from the satellites when 3 00:00:07.400 --> 00:00:09.600 we stay zoomed in. Not much to look at, not 4 00:00:09.600 --> 00:00:15.967 much to explore. It looks like just a 5 00:00:15.967 --> 00:00:18.867 smoothed out minor bump, and when you actually 6 00:00:18.867 --> 00:00:21.133 get down to brass tacks and get the high 7 00:00:21.133 --> 00:00:24.633 resolution data, just fascinating topography. 8 00:00:24.633 --> 00:00:27.333 And that's just simply one of the most fun 9 00:00:27.333 --> 00:00:29.633 things about doing the mapping of these 10 00:00:29.633 --> 00:00:32.533 seamounts is you have no clue what the surface is 11 00:00:32.533 --> 00:00:34.533 going to look like until you map it, and then 12 00:00:34.533 --> 00:00:37.033 once you map it, you're imagination just goes 13 00:00:37.033 --> 00:00:44.467 crazy. It's like being a little child again. Last 14 00:00:44.467 --> 00:00:46.800 year the Okeanos Explorer mapped a little 15 00:00:46.800 --> 00:00:50.033 over twenty percent of the monument and mapped 16 00:00:50.033 --> 00:00:53.233 three seamounts that had never been mapped 17 00:00:53.233 --> 00:00:57.367 before. Just last night we came upon a seamount 18 00:00:57.367 --> 00:01:01.500 that we did not know existed, and these are 19 00:01:01.500 --> 00:01:04.633 enormous features. Some of these seamounts that 20 00:01:04.633 --> 00:01:07.100 we just recently discovered are over ten 21 00:01:07.100 --> 00:01:10.300 thousand feet in height. For those in Hawaii, 22 00:01:10.300 --> 00:01:12.933 that's kinda like finding Haleakala that 23 00:01:12.933 --> 00:01:14.933 we didn't know existed.