Geological Insights from Malaysia Airlines Flight MH370 Search
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(360/0.25)*180 =~ 250 billion AU$
That's around 190 billion USD, not even 0.1 Iraq wars, and that's before considering any economies of scale.1. https://www.theguardian.com/world/2017/jan/17/malaysia-airli...
The annual budget for the entire USGS is $1.2 billion. NOAA has a budget of $5.6 billion. NASA has a budget of $19.5 billion. The NSF has a budget of about $2 billion. If these agencies dropped everything else and invested purely in this map, it would take about 5 years to create it.
Or, yeah, you could buy not even 0.1 Iraq wars with those 5 years, if that sounded better...
There is also the opportunity cost to take account of, but that's much harder (impossible?) to put an accurate figure on.
Nasa has been able to pull off the Apollo program for roughly $150B adjusted for inflation. Those are not real dollars neither because people supported it ?
There aren't that many multibeam sonar vessels in the world. They acquire data over narrow swaths. Mapping all ocean basins with multibeam would take a long time. I've always heard estimates of a few hundred years, though those were based on total the number of academic multibeam vessels operating 24/7. Obviously, it scales with the number of vessels you have doing it, so a large-scale coordinated effort that built lots of new, single-purpose vessels could take significantly less.
At any rate, the cost of one survey made with one ship is not a good way to estimate the total cost, unless you're willing to wait a _really_ long time.
A better application of money than redoing work already done, might be talking the navy into releasing their data. Declassification isn't cheap, but its cheaper than having civilians re-run the mission.
The vast majority of the ocean hasn't been mapped with multibeam, civilian or military. Unless it's an area that's of strategic interest (i.e. mostly costal areas), it's very unlikely that the military has mapped it in detail.
That having been said, getting the military to declassify more of its magnetic anomaly data for the ocean basins would be immensely helpful for understanding global tectonic evolution. They have mapped it in quite a bit of detail from airborne and marine platforms. However, an accurate and detailed map of magnetic anomalies gives a huge edge in submarine detection, so it's unlikely they'll declassify all of it anytime soon.
https://eos.org/opinions/airline-flight-paths-over-the-unmap...
190 million :)
It's still really quite amazing how well it matches in an area that's pretty far from dense ship-track bathymetry data.
And then the article became all the more sweeter when I realised that it all this work was done by people I know at Geoscience Australia. Very cool.
And we've just started an engineering blog which might be of interest to the HN crowd: https://tech.ga.gov.au
EDIT: found a lot more info (and videos) here : http://www.ga.gov.au/about/projects/marine/mh370-bathymetric...
Most of the deep ocean basins have absolutely zero oil.
To create thermogenic hydrocarbons, you need thick sediments. You can make methane biogenically without significant sediment cover, and that's important sometimes, but you cannot make oil that way. Oil is what drives exploration far away from population centers.
The abyssal plain you're seeing in that data is mostly exposed oceanic crust. There's almost no sediment cover. No sediments --> no exploration potential.
There's one narrow continental fragment that could have significant sediment cover. However, it's highly unlikely that that's prospective. (If you're curious, I'm happy to elaborate, but it will take a bit of explanation.)
There is one way this data will be used for petroleum exploration. It aids our understanding of the tectonic evolution of the area, which in turn aids petroleum exploration. However, if you're going to take a moral stance against that, you also need to a moral stance against every scientific advance in every field. They all aid the oil industry indirectly. (Ditto for software.)
For the more general geology portion, if you're wanting something that's a bit more detailed, but still very approachable, "Evolution of the Earth" by Prothero and Dott is absolutely fantastic. You can probably find a slightly older paperback edition quite cheaply, as well.
If you're really okay with a quantitative approach, Turcotte & Schubert's "Geodynamics" walks through an impressive amount of basic tectonics in a "let's do the back of the envelope calculations" manner. It's the most dog-eared book on my shelf. It's incredibly useful. However, it's a graduate level textbook, and it assumes you have at least a basic understanding of geological processes and terminology. It would be a very tough way to dive in.
Why isn't there sediment cover in these areas? I would naively think that you'd get some raining down as plants and animals die in the shallower depths. Clearly that must not be the case, but why not?
Additionally, oceanic crust is always very young geologically. It's continually formed and destroyed (subducted). The ocean basins haven't had much time to fill up with sediment, because oceanic crust is essentially a conveyor belt.
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So the short answer is: You're depositing things very slowly on something that doesn't have much time for sediments to build up.
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In a bit more detail, the sediments you get in the middle of the ocean are either the initial volcanic-related sediments that were deposited as the oceanic crust formed, or they're limited to "pelagic rain" (things near the surface dying and very fine particles of clay) and some chemical sediments (things that precipitate directly out of water).
Not only that, but a lot of the things that die and sink will dissolve below about 2 Km water depth (see Carbonate Compensation Depth).
Therefore, deepwater depositional rates are very, very slow.
There's a very important exception, though -- Carbonates. If you start in shallow water (say, due to a small sliver of continental crust), organisms in the photosynthetic zone can produce huge amounts of carbonate sediments just from their shells (e.g. coral reefs).
Under the right conditions, carbonates can keep growing and keep pace with the subsiding crust. A good example of this is the Bahamas. You have several kilometers of sediment made of nothing but what grew there and died. There are some very significant oil fields in these sorts of "isolated platforms".
However, you need fairly unique conditions to get oil in the sort of isolate carbonate platforms that develop far away from land. In most cases you'd find out in the ocean basins, you won't have a source rock capable of generating hydrocarbons beneath the pile of sediments that the carbonates produce. Instead, the source rock is conveniently sitting out there in the deep water where it's not buried deep enough to produce oil.
There's one other exception, and that's when you're near a volcano. Volcanoes will happily produce lots of volcanic-related sediments. However, volcaniclastic sediments almost never make good reservoirs (there are exceptions) or seals, so even if you did generate oil in a narrow band around a seamount, it would either leak out (no seal) or be trapped in something that you can't get it out of (bad reservoir).
And there's the longer answer :)