Skip to main content

Advertisement

Log in

Support for the Giant Wave Hypothesis: evidence from submerged terraces off Lanai, Hawaii

  • Original paper
  • Published:
International Journal of Earth Sciences Aims and scope Submit manuscript

Abstract

The origin of subaerial coral conglomerate deposits on the Hawaiian islands of Lanai and Molokai is controversial, primarily because these deposits are difficult to interpret and the vertical motion of these islands is poorly constrained. Based on bathymetry, dive observations, sedimentary and radiocarbon data from coralline algal dominated deposits from two submerged terraces at −150 and −230 m off Lanai, Lanai has experienced relatively little vertical movement over the last 30 ka. Using internally consistent age versus depth relationships, paleowater depths, and published sea level data, we estimate that Lanai has experienced maximum rates of uplift of 0.1 m/kyr or subsidence of 0.4 m/kyr over this period. Our analysis of possible uplift mechanisms, published geophysical, numerical modelling, and recent tide data suggests that this is also the maximum uplift rate for the last several hundred thousand years. Taken together these data support the interpretation that coral conglomerates at elevations higher than +35 m on Lanai are tsunami deposits with a minimum wave run up > 170 m, rather than shoreline deposits formed during the last two interglacials, then uplifted to their present elevations.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4

Similar content being viewed by others

References

  • Bard E, Hamelin B, Fairbanks RG (1990) U-Th ages obtained by mass spectrometry in corals from Barbados: sea level during the past 130,000 years. Nature 346:456–458

    Article  Google Scholar 

  • Camoin GF, Montaggioni LF, Braithwaite CJR (2004) Late glacial to post glacial sea levels in the Western Indian Ocean. Mar Geol 206:119

    Article  Google Scholar 

  • Campbell JF (1986) Subsidence rates for the Southeastern Hawaiian islands determined from submerged terraces. Geo-Mar Lett 6:139–146

    Article  Google Scholar 

  • Cutler KB, Edwards RL, Taylor FW, Cheng H, Adkins J, Gallup CD, Cutler PM, Burr GS, Bloom A (2003) Rapid sea-level fall and deep-ocean temperature change since the last interglacial period. Earth Planet Sci Lett 206:253–271

    Article  Google Scholar 

  • Fairbanks RG (1989) A 17000 year glacio-eustatic sea-level record: influence of glacial melting rates on the Younger Dryas event and deep ocean circulation. Nature 342:637–642

    Article  Google Scholar 

  • Felton AE, Crook KAW, Keating BH, Kay AE (2006) Sedimentology of rocky shorelines: 4. Coarse gravel lithofacies, molluscan biofacies, and the stratigraphic and eustatic records in the type area of the Pleistocene Hulopoe Gravel, Lanai, Hawaii. Sediment Geol 184:1

    Article  Google Scholar 

  • Galewsky J, Silver E, Gallup CD, Edwards L, Potts D (1996) Foredeep tectonics and carbonate platform dynamics in the Huon Gulf, Papua New Guinea. Geology 24:819–822

    Article  Google Scholar 

  • Grigg RW, Jones A (1997) Uplift caused by lithospheric flexure in the Hawaiian Archipelago as revealed by elevated coral deposits. Mar Geol 141:11–25

    Article  Google Scholar 

  • Hildenbrand A, Gillot P-Y, Bonneville A (2006) Offshore evidence for a huge landslide of the northern flank of Tahiti-Nui (French Polynesia). Geoch Geophys Geosyst 7. DOI:10.1029/2005GC001003

  • Johnson C, Mader CL (1994) Modeling of the 105 ka Lanai tsunami. Sci Tsunami Hazards 12:33–38

    Google Scholar 

  • Keating B, Helsley C (2002) The ancient shorelines of Lanai, Hawaii, revisted. Sediment Geol 150:3–15

    Article  Google Scholar 

  • Labazuy P (1996) Recurrent landsliding events on the submarine flank of Piton la Fournaise volcano (Reunoin Island). In: Mcguire WJ, Jones AP, Neuberg J (eds) Volcano instability on the Earth and other planets, vol 110. Special Publication of Geological Society. London, pp 293–306

  • Lambeck K, Chappell J (2001) Sea level change through the last glacial cycle. Science 292:679–686

    Article  Google Scholar 

  • Lambeck K, Esat T, Potter E (2002) Links between climate and sea-levels for the past three million years. Nature 419:199–206

    Article  Google Scholar 

  • Lea DW, Martin PA, Pak DK, Spero HJ (2002) Reconstruction a 350 ky history of sea-level using planktonic Mg/Ca and oxygen isotope records from a Cocos Ridge core. Quat Sci Rev 283:283–293

    Article  Google Scholar 

  • Lipman PW, Normark WR, Moore GJ, Wilson JB, Gutmacher C (1988) The giant submarine Alika debris slide, Mauna Loa, Hawaii. J Geophys Res 93:4279–4299

    Google Scholar 

  • Ludwig KR, Szabo BJ, Moore JG, Simmons KR (1991) Crustal subsidence rate off Hawaii determined from 234U/238U ages of drowned coral reefs. Geology 19:171–174

    Article  Google Scholar 

  • McMurtry GM, Herrero-Bervera E, Cremer M, Resig J, Sherman CE, Smith JR, Torresan ME (1999) Stratigrahic constraints on the timing and emplacement of the Alika 2 giant Hawaiian submarine landslide. J Volcanol Geotherm Res 94:35–58

    Article  Google Scholar 

  • McMurtry GM, Fryer GJ, Tappin DR, Wilkinson IP, Williams M, Fietzke J, Garbe-Schoenberg D, Watts P (2004a) Megatsunami deposits on Kohala volcano, Hawaii, from flank collapse of Mauna Loa. Geology 32:741–744

    Article  Google Scholar 

  • McMurtry GM, Watts P, Fryer GJ, Smith JR, Imamura F (2004b) Giant landslides, mega-tsunamis, and paleo-sea level in the Hawaiian Islands. Mar Geol 203:219–233

    Article  Google Scholar 

  • Moore AL (2000) Landward fining in onshore gravel as evidence for a late Pleistocene tsunami on Molokai, Hawaii. Geology 28:247–250

    Article  Google Scholar 

  • Moore JG, Fornari DJ (1984) Drowned reefs as indicators of the rate of subsidence of the island of Hawaii. J Geol 92:753–759

    Google Scholar 

  • Moore JG (1987) Subsidence of the Hawaiian Ridge. In: Decker RW, Wright TL, Staufer PH (eds) Volcanism in Hawaii, vol 1350. U.S. Geological Survey Professional Paper, Washington, pp 85–100

  • Moore GW, Moore JG (1984) Deposit from a giant wave on the islands of Lanai, Hawaii. Science 226:1312–1315

    Article  Google Scholar 

  • Moore GW, Moore JG (1988) Large-scale bedforms in boulder gravel produced by giant waves in Hawaii. In: Clifton HE (ed) Sedimentologic consequences of convulsive geologic events, vol 229. Geological Society of America Special Paper, pp 101–110

  • Moore JG, Clague DA, Holocomb RT, Lipman PW, Normark WR, Torresan ME (1989) Prodigous submarine landslides on the Hawaiian Ridge. J Geophys Res 94:17465–17484

    Google Scholar 

  • Moore JG, Clague DA, Ludwig KR, Mark R (1990) Subsidence and volcanism of the Haleakala Ridge, Hawaii. J Volcanol Geotherm Res 42:273–284

    Article  Google Scholar 

  • Moore JG, Bryan WB, Ludwig KR (1994) Chaotic deposition by a giant wave, Molokai, Hawaii. Geol Soc Am Bull 106:963–967

    Google Scholar 

  • Moore JG, Bryan WB, Beeson MH, Normark WR (1995) Giant blocks in the South Kona landslide, Hawaii. Geology 23:125–128

    Article  Google Scholar 

  • Morgan E, Day S, Elemunop J, Silver E, Ward S, Hoffmann G (2005) Tsunami deposits related to volcanic Island collapses in the Southern Bismarck Sea. Eos Trans AGU 86 (52), Fall Meet Suppl, Abstract V21B-0600

  • Muhs DR (2002) Evidence for the timing and duration of the last interglacial period from high-precision Uranium-series ages of corals on tectonically stable coastlines. Quat Res 58:36–40

    Article  Google Scholar 

  • Rubin KH, Fletcher CH III, Sherman C (2000) Fossiliferous Lana’i deposits formed by multiple events rather than a single giant tsunami. Nature 408:675–681

    Article  Google Scholar 

  • Silver E, Day S, Ward S, Hoffmann G, Llanes P, Lyons A, Driscoll N, Perembo R, Applegate B, Engels J, Smith J, Tagliodesm J (2005) Island arc debris avalanches and tsunami generation. EOS Trans Am Geophys Union 86:485–489

    Google Scholar 

  • Smith JR, Wessel P (2000) Isostatic consequences of giant landslides on the Hawaiian Ridge. Pure Appl Geophys 157:1097

    Article  Google Scholar 

  • Stearns HT (1966) Geology of the state of Hawaii. Pacific Books, Palo Alto

    Google Scholar 

  • Stearns HT (1978) Quaternary shorelines in the Hawaiian Islands. Bernice P. Bishop Mus Bull 237:57

    Google Scholar 

  • Szabo BJ, Ludwig KR, Muhs DR, Simmons KR (1994) Thorium−230 ages of corals and duration of the last interglacial sea-level highstand on Oahu, Hawaii. Science 266:93–96

    Article  Google Scholar 

  • Ward SN, Day S (2001) Cumbre Vieja Volcano—potential collapse and tsunami at La Palma, Canary Islands. Geophys Res Lett 28:3397–3400

    Article  Google Scholar 

  • Ward SN, Day SJ (2003) Ritter Island Volcano—lateral collapse and tsunami of 1888. Geophys J Int 154:891–902

    Article  Google Scholar 

  • Watts AB, ten Brink US (1989) Crustal structure, flexure, and subsidence history of the Hawaiian Islands. J Geophys Res 94:10473–410500

    Google Scholar 

  • Webster JM, Clague DA, Riker-Coleman K, Gallup C, Braga JC, Potts D, Moore JG, Winterer EL, Paull CK (2004a) Drowning of the −150 m reef off Hawaii: a casualty of global meltwater pulse 1A? Geology 32:249–252

    Article  Google Scholar 

  • Webster JM, Wallace L, Silver E, Potts D, Braga JC, Renema W, Riker-Coleman K, Gallup C (2004b) Coralgal composition of drowned carbonate platforms in the Huon Gulf, Papua New Guinea; implications for lowstand reef development and drowning. Mar Geol 204:59–89

    Article  Google Scholar 

  • Webster JM, Clague DA, Braga JC, Spalding H, Renema W, Kelley C, Applegate B, Smith JR, Paull CK, Moore JG, Potts D (2006) Drowned coralline algal dominated deposits off Lanai, Hawaii; carbonate accretion and vertical tectonics over the last 30 ka. Mar Geol 225:223–246

    Article  Google Scholar 

  • Wessel P (1993) A reexamination of the flexural deformation beneath the Hawaiian Islands. J Geophys Res 87:12177–112190

    Article  Google Scholar 

  • Wessel P, Keating B (1994) Temporal variations of flexural deformation in Hawaii. J Geophys Res B Solid Earth Planets 99:2747–2756

    Article  Google Scholar 

  • Yokoyama Y, Lambeck K, De Deckker P, Johnson DP, Fifield LK (2000) Timing of last glacial maximum from observed sea-level minima. Nature 406:713–716

    Article  Google Scholar 

  • Zhong S, Watts AB (2002) Constraints on the dynamics of mantle plumes from uplift of the Hawaiian Islands. Earth Planet Sci Lett 203:105

    Article  Google Scholar 

Download references

Acknowledgments

We acknowledge the support of the David and Lucile Packard Foundation through a grant to MBARI. We are grateful to Gilbert Camoin, Yasufumi Iryu, Simon Day and two anonymous reviewers for their very constructive comments which improved the manuscript.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Jody M. Webster.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Webster, J.M., Clague, D.A. & Braga, J.C. Support for the Giant Wave Hypothesis: evidence from submerged terraces off Lanai, Hawaii. Int J Earth Sci (Geol Rundsch) 96, 517–524 (2007). https://doi.org/10.1007/s00531-006-0107-5

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00531-006-0107-5

Keywords

Navigation