3 ms·
The top of the magma chamber starts ~5-17 km from the surface with another magma chamber ~20-50 km from the surface. Heat starts and goes well above that of cou
by zamadatix 2y ago
The top of the magma chamber starts ~5-17 km from the surface with another magma chamber ~20-50 km from the surface. Heat starts and goes well above that of course but if your goal is to meaningfully hook into and extract the heat of the chamber itself it's quite deep. Put from another perspective: if a significant amount of the energy of the chamber were imminently near the surface it would already fizzle itself out over thousands of years without the need of digging short holes to do it in a few.
Geothermal in Yellowstone is no better or more useful than geothermal at many other less important places. It isn't even the place with the most surface level geothermal energy in the first place. Overall geothermal technology advancement makes a lot of sense but starting said advancement via sandbagging for an outcome 1000 years after developing one of the best national parks to do so does not make sense.
Regardless of all of that, there are significantly more than the two possibilities of either starting drilling today or having catastrophe in an eruption.
- OutOfHere 2y agoThe reason why I noted a thousand year period is because Yellowstone is said to have a lot more energy than we can use right now. Regarding the investment, if a 5 km well is dug, I don't expect it to exhaust its energy without a significant payback.
- dredmorbius 2y agoAFAIU the "last mile" (or last 5--17 km) transfer largely occurs through ground-water migration. Yellowstone combines extensive geothermal energy with ample surface water flow (e.g., Lake Yellowstone, which is itself a major geothermal zone). I'm really well beyond my depth here, though looking up soem background: Geological diagram of Old Faithful: <https://public-media.smithsonianmag.com/filer/bd/06/bd0603df-a976-44b2-9300-5936c3b5eb52/ofdiagram.jpg https://public-media.smithsonianmag.com/filer/bd/06/bd0603df...> From this Smithsonian article: <https://www.smithsonianmag.com/smart-news/seeing-beneath-old-faithful-180965230/ https://www.smithsonianmag.com/smart-news/seeing-beneath-old...> "Old Faithful's Geological Heart Revealed": <https://www.sciencedaily.com/releases/2017/10/171005190243.htm https://www.sciencedaily.com/releases/2017/10/171005190243.h...> Mostly addresses seismic activity, though there's some discussion of inferred structures from that. Based on the journal article by Sin-Mei Wu, Kevin M. Ward, Jamie Farrell, Fan-Chi Lin, Marianne Karplus, Robert B. Smith. "Anatomy of Old Faithful from subsurface seismic imaging of the Yellowstone Upper Geyser Basin". Geophysical Research Letters, 2017; DOI: 10.1002/2017GL075255 <http://dx.doi.org/10.1002/2017GL075255 http://dx.doi.org/10.1002/2017GL075255> (The Smithsonian piece is based on the same article.)
- OutOfHere 2y agoExactly. I am not convinced that drilling 5 km is necessary at Yellowstone. I suspect the energy is ripe for the taking much closer to the surface due to this water migration.