Kilauea’s south flank slumping is “normal” – I’m so much relieved now…

From the “How not to console” department…

In order to assure folks that the area of the Leilani Eruption of Kilauea is NOT going to slide off into the sea, the USGS explains that it is only “slumping” slowly into the ocean in a more normal way and that won’t cause a tsunami at all.

https://volcanoes.usgs.gov/observatories/hvo/hvo_news_archive.html

Bold bits bolded by me.

Facts on the stability of Kilauea’s south flank, past and present.
May 14, 2018

There have been several recent highly speculative stories, rumors and blogs about the stability of the south flank of Kilauea and the potential for a catastrophic collapse that could generate a Pacific-wide tsunami. We wish to put these speculations in their proper context by presenting observations of the current situation and an assessment of past evidence of landslides from Kilauea.

There is no geologic evidence for past catastrophic collapses of Kilauea Volcano that would lead to a major Pacific tsunami, and such an event is extremely unlikely in the future based on monitoring of surface deformation. Kilauea tends to “slump”, which is a slower type of movement that is not associated with tsunamis, although localized tsunamis only affecting the island have been generated by strong earthquakes in the past.

Oh, so it won’t land slide it will only land slump; I’m so much relieved. No tsunami for California then.

The May 4 M6.9 earthquake resulted in seaward motion of approximately 0.5 m (1.5 ft) along portions of Kilauea’s south flank as measured by GPS stations across the volcano. A preliminary model suggests that the motion was caused by up to 2.5 meters (8 feet) of slip along the fault that underlies the volcano’s south flank, at the interface between the volcano and the ocean floor, about 7-9 km (4-6 mi) beneath the surface. This motion is within the expected range for a large earthquake on this fault. The earthquake was probably caused by pressure exerted by the magmatic intrusion on the south flank fault, following the pattern of past earthquake activity that has been observed during Kilauea East Rift Zone intrusions. A small, very localized tsunami did occur as a result of the fault slip. Similar local tsunamis were generated by past large earthquakes, including the 1975 M7.7 and 1868 ~M8 events, both of which resulted in multiple deaths along the south coast of the Island of Hawaii.

Hey, it’s only moved 1.5 feet at the surface ( 2.5 meters or 8 feet down at the actual fault ). It’s only a 5 mile +/- thick slab doing the “slump” anyway… And it is “expected”. We all know that if you “expect” at tornadoes and hurricanes they don’t hurt you either, so why would a volcano be any different? We ALL need to get our attitude straight and start “expecting” at the volcano so it acts nice. (While we are at it, remember that this power of “expecting” is likely why the Global Warmistas hate the Deniers – it is all our fault for not properly “expecting” Global Warming, as clearly failure to “expect” enough lets The Bad Thing happen… /sarc;)

I also like the way they point out that the lava flowing into the dikes is acting as a hydraulic ram sliding that slab over “caused by pressure exerted by the magmatic intrusion”. So I guess we just hope that the pressure stays constant? No, that’s making it move… We hope that the pressure decreases? I really need to know what I’m supposed to “expect” so I can do my proper job of expecting to keep The Bad Thing away.

Adjustments on the south flank caused another ~9 cm (3.5 inches) of motion at the surface in the day after the earthquake, followed by another 2-3 cm (~1 inch) since May 5. This is higher than the normal rate of south flank motion (~8 cm (3 inches) per year) but is expected as the volcano adjusts after a combination of a magmatic intrusion along the East Rift Zone and a large south flank earthquake. We did observe minor ground ruptures on the south flank, but this is expected given the strength of the May 4 earthquake, and deformation data show that the south flank continues to move as an intact slump block.

Geologic history combined with models of south flank motion suggest that the likelihood of a catastrophic failure event is incredibly remote. There are certainly signs on the ocean floor for landslides from other volcanoes on the Island of Hawaii and from other islands, but none are associated with Kilauea. In addition, Kilauea has experienced much larger earthquakes and magmatic intrusions in the recent past. The large earthquakes of 1975 and 1868 were not associated with significant south flank landsliding, nor were major East Rift Zone intrusions in 1840 and 1924.

So it’s normally “slumping” some every year, and it did speed up with the quakes and the lava and all, but it, too, is “expected”. Oh, and I’m Sooooo happy to know that “the south flank continues to move as an intact slump block” and is not breaking up as it “slumps” toward the sea. And as long as we don’t have too many earthquakes, it will be slow enough nobody will notice. Well, other than the fissures and the lava and all… but that’s “expected”…

Besides, all the OTHER SLUMP failures into the ocean and the landslides of massive chunks causing huge tsunami events have only happened “from other islands” and “none are associated with Kilauea”. So just ’cause the other islands and volcanoes do it doesn’t mean this one will do it… well, at least not now. It’s just not expected now. (One hopes this lack of expecting does not let this Bad Thing sneak past the expectation barriers protecting the Big Island…)

So no worries, eh? This is just the volcanoes way of getting a little wiggle room for it’s fissure toes. Just gently shoving a few miles thick section of flank over a little bit, just a few meters, making room for some more island below the surface. I mean, it’s a feature, don’t you see? Otherwise all that lava would have to flow over the surface to get more room for more island. We’ve seen how that works out. ( I guess not enough folks were expecting it… Bad Tourists!)

http://www.science-frontiers.com/sf115/sf115p09.htm

The hilina slump a.k.a. “the big crack”

Huge chunks of the Hawaiian Islands have been sliding into the Pacific Ocean for hundreds of thousands of years.
(SF#101) Geologists classify these slides as either “slumps” or “debris avalanches.” Slumps move just a few inches a year but are prone to bigger, jerky adjustments. Debris avalanches are fast cascades of rocks and soil. In Hawaii, both varieties of movement can involve massive blocks of real estate. In the huge Nu’uanu debris slide, stone blocks 6 miles across tumbled 30 miles out to sea. Both slumps and debris slides may create colossal tsunamis. (Tsunamis are miscalled “tidal waves,” but they have nothing to do with tides and do not behave like tides or wind-driven waves.)

When large pieces of the Hawaiian Islands slip into the ocean, the entire Pacific Rim is smashed by the resulting tsunamis. In New South Wales, Australia, there is geological evidence that part of this coast was scoured by a Hawaii generated tsunami 100,000 years ago. The postulated wave started out about 375-meters (½-mile) high in Hawaii. By the time is reached Australia, it was about 40 meters high. (SF#85)

Worse waves may be on tap. A 4,760 cubic mile chunk of the Big Island (Hawaii) is breaking away at the rate of 4 inches per year. This is the Hilina Slump, and it is said to be “the most rapidly moving tract of ground on Earth for its size.” The Hilina Slump can move much faster. At 4:48 AM, November 29, 1975, a 37-mile-wide section suddenly dropped 11½ feet and slid seaward 26 feet. The result was a magnitude-7.2 quake and a 48-foot-high tsunami. This was a minor of the slump. If the entire 4,760-cubic-mile block decided to break off, it would probably create a magnitude-9 quake and a tsunami 1,000-feet high. All the coast-hugging cities of the Hawaiian Islands would be swept away. And LOOK OUT Australia, Japan, and California.

(Napier, A. Kam; “Landslide,” Honolulu, p. 28, February 1997. Cr. H. DeKalb.)

But no reason to expect that. It isn’t likely. Not right now. It will only be likely after is has a sudden “jerky adjustment”.

http://channel.nationalgeographic.com/a-night-of-exploration/articles/drain-the-ocean-facts/

The Nu’uanu debris avalanche contains enormous blocks ~30 km long, 17 km wide, and at least 2 km tall. The landslide is spread over a 23,000 km2 area.

The Tuscaloosa seamount or debris from the Nu’uanu debris slide is one mile deep and over 135 m2 in area. This rivals the size of the city of Atlanta.

Nu’uanu debris extending 150 miles from the island is the size of the state of New Hampshire.

Scientists have identified over fifteen giant landslides surrounding the Hawaiian Islands.

http://www.soest.hawaii.edu/GG/FACULTY/garcia/publications/Garcia%20et%20al%2006%20ODP200%20slides.pdf

Frequent landslides from Koolau Volcano: Results
from ODP Hole 1223A
Michael O. Garcia, Sarah B. Sherman, Gregory F. Moore, Robert Goll, Irina Popova-Goll, James H. Natland, Gary Acton

Accepted 15 July 2005
Available online 16 November 2005

Abstract

Giant landslides on the flanks of oceanic islands are considered relatively rare but potentially devastating natural hazards. The Hawaiian Islands are known to produce some of the biggest landslides on Earth. The Nuuanu slide, largest of the Hawaiian slides, is thought to have removed a substantial part of Koolau Volcano from the island of Oahu. Ocean Drilling Program (ODP) Hole 1223A was drilled to determine the depositional history, timing, thickness and hazards associated with the Nuuanu landslide, the only previously known Koolau slide. Site 1223, located ~260 km northeast of the island of Oahu near the crest of the 500-m-high Hawaiian Arch, was drilled to a depth of 41 m. Eight distinct sandy layers were recovered and more are likely to occur deeper in the section. Contacts of these sandy layers with pelagic clay are sharp at their base and gradational at the top. The layers contain angular fresh glass fragments with compositions that are typical of Hawaiian shield volcanoes, including the distinctive Koolau high SiO2-type in seven layers. Most glasses ( > 90%) are degassed ( < 0.03 wt.% S) indicating that they were probably erupted subaerially. Pleistocene to Early Eocene Radiolaria taxa are present in the Hole 1223A cores, with mixed ages in some intervals. Seven of the sand layers are probably associated with Koolau landslides and were deposited prior to 1.77 Ma. Among the four thicker sand layers ( > 1.5 m), it is unclear which, if any, are related to the Nuuanu slide. Results from Hole 1223A cores demonstrate that Hawaiian volcanoes collapse repeatedly, and the debris from these many slides can travel great distances ( > 260 km) across the ocean floor and over significant bathymetric obstacles (~500 m). Thus, landslides from oceanic volcanoes pose a greater risk than previously assumed.

But just because they are a regular feature of the Hawaiian Islands and “pose a greater risk than previously assumed” and happen repeatedly as the islands age and the basaltic rock weathers; that’s no reason to expect them. After all, these things happen on geologic time scales. The odds are quite small in any one decade, or even century. Nearly zero in fact. Until it happens.

Subscribe to feed

Advertisements

About E.M.Smith

A technical managerial sort interested in things from Stonehenge to computer science. My present "hot buttons' are the mythology of Climate Change and ancient metrology; but things change...
This entry was posted in News Related and tagged , , , , . Bookmark the permalink.

34 Responses to Kilauea’s south flank slumping is “normal” – I’m so much relieved now…

  1. philjourdan says:

    The picture in the first link is deceptive. While we may not be in “danger” of a catastrophic slide causing a Tsunami in the near future, the picture shows a very gradual shelf off the coast which we know to be false. Hawaii is the tallest mountain in the world (measured base to summit), and the drop off is much more pronounced. Thus a “slide” (or rapid “slump”) would not be like someone slipping into a bath tub, but rather like Hamilton Porter’s cannon ball.

    What we do know about the Hawaiian islands is that all of them were created by basically the same magma plume. The crust just keeps moving so it creates new islands. So why is Hawaii the largest? Are we just lucky that the crust has lingered longest in recent times?

    Doubtful. We do know that Molokai was not always a sliver, but at one time a nice plump island. But most of it slipped below the waves long before recorded history. With the new information about Oahu, that seems to be the norm, not the exception.

  2. John F. Hultquist says:

    These volcanoes are not the sort that tend to explode like Mount St. Helens or Pinatubo. I think the words “expected” and “normal” are misused. These things are episodic and each event changes things for the next time. I’d coin a new term: eposotic, thereby including the notion of exotic in the description. That is, something we don’t expect might happen.
    What bothers me – – Why are all those people living there on the most dangerous side of an active volcano?
    And, how much is this going to cost American tax payers?

    Related, but haven’t seen this discussed recently:
    There has been a vent forming a new island, Loihi Seamount (still below the ocean surface) about 20 miles off the coast.

    Summary here:
    https://geology.com/usgs/loihi-seamount/

    USGS document here:
    https://pubs.er.usgs.gov/publication/gip117

    All quite fascinating examples of a dynamic Earth.

    I live 66 miles east of Mt. Rainier, and 177 miles east of the Pacific Coast. Both of these places can produce dangerous and quite sudden actions. Mt. Rainier will give a warning, analogous to a rattlesnake. The Bald-faced Hornet attack would be the Cascadia Subduction Zone. It is likely to just “go” with almost no warning. [After the fact, a warning might be recognized, for next time.]

  3. Larry Ledwick says:

    I saw a comment that the reason people live there is the land is cheap for obvious reasons.
    If you are not rich about the only place you can live on Hawaii.

  4. E.M.Smith says:

    You pays yur money and ye take yur chances…

    On top of the slope, you need to worry a bit about the occasional big eruption from the top. Unlikely in any given century, but it happens (that comment about this being a little hole in a BIG caldera…).

    On the bottom of the slope / shore, you also need to worry a bit about he occasional big eruption, but can hop in your boat and get away. You also must pay $Million scale price tags and fight with megaresorts for land.

    Used to be on the Kona side there were modest priced farming communities. About ’70s or so, developers figured they could haul in sand and make beaches and grade the lava fields. Now it is expensive tourist land too… There is still some ranching if you head right (east? North? Anti-clockwise…) out of Hilo, yes, ranches, as in cattle; but they have very little water.

    That basically leaves Hilo, a great town where we had 1/4 of our honeymoon, on the water and relatively safe from “expected” activity. BUT in geologic time scale eruptions you will get lava. (There’s a great little Fish Farm right on the coast that is fed COLD water from snow melt up on the mountain… they farm TROUT in it!… But that also means an old lava tube runs from up on the mountain to there…)

    In geologic time (hundreds of thousands to millions of years) Kilauea will become dormant as the “New Island” takes over the hot spot and the next island forms. Then Hawaii (the Big Island) will start the long slumping decay into smaller bits until it fades away at the far end of the chain like Kauai then Midway…

    I’d be happy to live in Hawaii… as long as I could own a big boat…

  5. philjourdan says:

    There’s the boat hook again! ;-)

  6. oldbrew says:

    Just another alarmist fail then.

  7. Graeme No.3 says:

    E.M.S.
    “He believes that, …., six big tsunamis caused by meteorite strikes or marine landslides have hit Sydney during the past 10,000 years. The most recent probably occurred in 1491, …, and produced a wave that washed over the harbour’s headlands, 60 m above sea level.
    For recent history
    http://www.bom.gov.au/tsunami/history/index.shtml

    And where a tsunami would most affect (there’s a lot of very expensive real estate there).
    https://www.theaustralian.com.au/news/nation/nsw-tsunami-maps-show-where-sydney-would-need-to-be-evacuated/news-story/d8293fc09ccb261237f79ab768fe7c41

  8. E.M.Smith says:

    All I can say is that there’s a REASON all those islands looked like Virgin Islands when Polynesians arrived and then later when white guys got to some others.

    Every so often, something Really Really Big scours them clean.

    So go ahead and live there…. just check the Tsunami reports every day, at bed time and when you get up… and have a Big Boat ( get away from the land rise at shore and the tsunami is a nothing) or a private plane with no more than a 1 hour dispatch time…

  9. philjourdan says:

    And here I thought it was because they were in the middle of nowhere and no one had been able to find them. But yea, being scoured clean would do that as well.

  10. p.g.sharrow says:

    That “slump” has created a crack or void that is filling with melt and magma from the main vent. As soon as the voids are filled and the main vent begins to refill, it will hydraulic the crack and push or lift the top of the slump. There will be quake swarms as the slump starts to travel. This is a huge train and will take time to get it rolling. Look for increased elevation of lava fountains at the cracks as a first warning of the voids being full, the main vent beginning eruption out burst as it refills.
    I would be monitoring deformation just below that fault or fracture line for both linear and elevation changes.
    This may be a false start or might become a Pacific coast disaster of massive proportions. This could take a few days or millennia if the magma chamber fails to refill before cooling freezes the intrusion and temporarily locks the slip. I fear the worst…pg

  11. Larry Ledwick says:

    Looking at this elevation map a 300 ft tsunamii surge would (depending on how long it took to penetrate into the inner low lands) make a lot of central California wet. (initial height could be near 1600 ft near the slide)

    https://geology.com/topographic-physical-map/california.shtml

    Obviously you have to consider flow durations and the limitations of flow through choke points near the bay (you can only push so much water through the golden gate in the time the waves are at its high crests for each of its successive crests.)

    That said it would be a major disaster all along the pacific coast if it were to happen in our time.

  12. p.g.sharrow says:

    @Larry the drain of the central valley, the Sacramento River traverses a narrow defile through the Coast Range so there would be little flooding into the Central Valley. The Narrows of the Golden Gate would limit flooding within the bay, but the coastal flooding would make the Japan tsunami look like a tide surge. There is Geological evidence of 200 ft Tsunami Waves all up and down the Pacific Coast.
    I just talked to a friend that gathers interesting information. There are psychic indications of some major disaster, financial/physical, around September.. .pg

  13. Larry Ledwick says:

    Yes between the cascadia fault earthquakes and Alaska or Hawaii generated tsunamis, periodic coastal inundation along the pacific coast is pretty much a given.

    Too bad the public outside of the Vancouver risk area are not even aware of the risks.

  14. Larry Ledwick says:

    They are starting to see some ballistic boulder ejecta from the crater no so it may beginning to enter a steam explosion phase.

    https://www.reuters.com/article/us-hawaii-volcano/volcanic-smog-drifts-to-other-hawaii-islands-ash-carpets-towns-idUSKCN1IH2R6

  15. E.M.Smith says:

    There’s a 2 stage “choke” on the Central Valley. First is the Golden Gate. Water then spreads out over the bays (San Francisco, San Pablo different names to the two ends…) and it then runs into the next choke point more inland. At that point, water would have little force (Golden Gate taking the force out) and limited height (spreading over the bays and adjoining nearly flat lands) so what did make it through the Carquinez Strait would be little and facing a huge Central Valley. It would make a mess of the entire coastal area, somewhat mess up around the SF Bay, but be limited in effect past Stockton.

    https://en.wikipedia.org/wiki/Carquinez_Strait

    There’s layers of mountains between ocean and inland…

    I’m at about 60 foot / 20 meters elevation, inside the first bit of coastal mountains. I figure I’m likely good for about a 100 m tidal wave… it would make a mess of San Francisco, but as water spread out behind them the expansion ratio is well over 5:1 and I’m inland at the far end of the bay.

    That’s the hope anyway…

  16. Larry Ledwick says:

    Looks like Kilauea just went ballistic with a summit eruption generating a 30,000 foot plume and tossing large rocks into the surrounding area.

    https://www.zerohedge.com/news/2018-05-17/kilauea-erupts-explosively-summit-sending-huge-plume-ash-sky

  17. u.k.(us) says:

    The volcanologists are certainly learning a few of Her tricks now :)
    She only reveals them sparingly, She’s been at it a long time.

  18. E.M.Smith says:

    I’ve been watching the local Hawaiian news on the Roku. “NewsON” channel lets me watch local news from all over, including KHNL Honolulu Hawaii… The local coverage of the volcano is, as you might expect, pretty detailed and from folks generally cluefull about the local geology. They do tend to say a bunch of Hawaiian names fast and that can be a challenge sometimes, but mostly that’s when they are saying what roads and districts are impacted and which roads are open…

    Radar said something got shot up to 30,000 feet. I wonder just what initial velocity must be to get a glowing blob of molten rock to 30,000 feet… I could calculate the gravity part, but what’s the drag? Or is it shrouded in a shield of upwardly mobile “stuff”?

    Right now the are giving ash fall advisories and directions of what to do if in your car and suddenly get ashed.

    Looks like they have some rain at the moment…

    They say that there was ONE big ejection at 4 something AM, so no ash plume to show at the moment on video.

    UPDATE:

    Looks like they have a live feed on the internet too:

    http://www.hawaiinewsnow.com/category/198303/livestream

    NewsON has an App on the Google Store, Apple, Amazon, and then Roku:

    http://newson.us/

    The also have a ‘Trending’ list that includes the volcano and then search by categories… so looks like you can connect directly through their web site too. Special URL here:
    http://watchnewson.com/

  19. Larry Ledwick says:

    Some of their web cams for live views ( they also have a photo archive link)

    https://volcanoes.usgs.gov/volcanoes/kilauea/multimedia_webcams.html

  20. p.g.sharrow says:

    map of the effected area:

    good view of previous lava flows and buildup in the area of the present flows. This is nothing new in that place. Kilauea is a separate entity on the flank of Mona Loa, with it’s own vent supply from 60 miles below…pg

  21. Larry Geiger says:

    AccuWeather – “Many Hawaiians accept their fate at the hands of a fire, land-devouring goddess amid Kīlauea eruptions”. Eruptions in Hawaii do not devour land. They create land. Volcanic eruptions created the islands. Right?

  22. philjourdan says:

    @P.G. – the map you posted is very interesting in so far as the number of “creeks” (I am not sure you can call them rivers). It does demonstrate just how much rain the island gets to have so many on such a small piece of land.

  23. E.M.Smith says:

    @Phil:

    The Islands have a “wet side” and a “dry side”. The trade winds bring saturated humidity air ( 3000 miles of drifting over water) and it hits the mountain. Ridge Lift makes it drop the water. Back side of the mountain gets nothing.

    You can literally drive around the island and go from torrential rain to dry sun and back again.

    Kona side has resorts where the problem was always “no water”. Once they fixed that ( I think they used osmosis desalinizing) the resorts blossomed as it was “always sunny”. You drive over miles and miles of dead black volcanic rocks to get to them… Over on the Hilo side it’s all lush Tropical Rain Forrest and you get that whole ambiance. But pretty much any day it can be raining in the afternoon. Sort of like Florida that way. Warms up, rains, cools off.

    This particular volcano event is mostly toward the rainy side.

    On Kauai one spot gets 400 inches a year. Other side of the island is a desert… Choose your radius, choose your weather…

  24. E.M.Smith says:

    I should probably have said “choose your radius and elevation” as both matter. More lift, more water drop:

    The district that’s getting the fissures is near the bottom edge of blue area:

    Kona coffee comes from the yellow streak just on the other side from the blue blob, then just north of that where it gets very very red (desert) is where they planted resorts via tech. No rain meant little erosion so no beaches – answer: haul in lots of sand and make a beach. Use reverse osmosis to supply drinking water and irrigate palms and greenery with “gray water”… Instant Resort that never gets rained out…. “Kona Side” but a few miles up from the Kona Coffee and traditional villages. I like that area, BTW…

  25. E.M.Smith says:

    @ossqss:

    I think they are over reacting. The solvent is basically gasoline. Pentane IIRC. Yes, it is very flammable. But it is not mixed with air…

    So the most likely scenario is really a giant gas flair as the solvent boils and gets shot up into the air. The only way you could get an explosion would be a BLEV where the vapors mixed THEN ignited, but that would be a fireball in the sky, not underground, and would not make a tsunami.

    This is far less risky than a fire at an oil refinery, and about the same nature.

  26. philjourdan says:

    Thanks for the update on rain. While 20 inches is not great, it seems kind of strange to call it a desert (we only get 40 here, 50 in a wet year). But it is interesting to see the contrast in what still amounts to a small amount of land! I do not think Cacti would do well on the island, but Roses would!

  27. E.M.Smith says:

    P.G. has some really nice pictures, maps and video here:
    https://pgtruspace.wordpress.com/2018/05/18/kilauea-eruption-may-2018/

    This video shows the whole slumping thing, and the historical outflows that we know of around the islands. I knew of such a map but was too lazy to find it…

    So hit the link, look at his stuff. It’s well done.

    FWIW, last I heard we were up to 21 or 22 fissures. The experts were a bit surprised that some of them had restarted heavy flows, and #17 in particular was going to town… (perhaps literally if this keeps up a few more weeks…)

  28. p.g.sharrow says:

    Early on it seemed to be “old lava” from the Kilauea lake that was spilling from the Rift, but now the chamber below is feeding “new” stuff into the area and the rift is widening. The Kilauea mound is subsiding as the chamber below deflates…pg

  29. E.M.Smith says:

    One wonders what will happen if the thing preventing lots of the hot zone ‘erupting’ was the weight of 4000 ft of molten rock in the stand pipe… that weight now relieved by a side tunnel to the fissures… IF much newer hotter magma flows well it can start to erode the whole channel larger for even freer flow…

Anything to say?

Fill in your details below or click an icon to log in:

WordPress.com Logo

You are commenting using your WordPress.com account. Log Out /  Change )

Google+ photo

You are commenting using your Google+ account. Log Out /  Change )

Twitter picture

You are commenting using your Twitter account. Log Out /  Change )

Facebook photo

You are commenting using your Facebook account. Log Out /  Change )

w

Connecting to %s

This site uses Akismet to reduce spam. Learn how your comment data is processed.