Post-1.8-ka Marginal Sedimentation in Lake Taupo, New Zealand

Effects of Wave Energy and Sediment Supply in a Rapidly Rising Lake

Nancy R Riggs, Michael H Ort, J. D L White, C. J N Wilson, B. F. Houghton, R. Clarkson

Research output: Chapter in Book/Report/Conference proceedingChapter

18 Citations (Scopus)

Abstract

The eruption of Taupo caldera, New Zealand, c. 1.8 ka, climaxed in the emplacement of the Taupo ignimbrite, which dammed the previous outlet of the caldera lake and allowed rise of the lake behind the dam to c. 34 m above current lake level. After an estimated 20 yrs of lake refilling, the ignimbrite dam was breached, and the lake drained rapidly to a position 2-4 m above current level. From that level, the lake apparently dropped slowly to its present position. Post-1.8-ka lacustrine sediments are exposed at various levels between the highstand and the modern shoreline. The distribution of lacustrine facies at Taupo reflects the location of the mouths of rivers that drained uplands buried and/or denuded of vegetation by the erupted material, together with the position of depositional sites with respect to prevailing winds and energy systems. Four broad facies environments can be recognized, defined by combinations of high or low energy and high or low sediment influx. Sediments deposited in areas of high energy (i.e. strong wave action) and high sediment input are rich in vitric material, but contain abundant lithic material in those deposits interpreted as storm influenced. Deposits in low-energy areas that had high sediment input are dominantly vitric, with abundant shoreface and pumice-raft deposits. High-energy, low-sediment-input areas are rich in lithic detritus, apparently reworked from ignimbrites along the pre-eruptive lake shore during storms. Deposits that characterize low-energy, low-sediment-input environments are poor in lithic detritus, reflecting the inability of currents to transport material to these sites. Terraces prominent above the modern shoreline of Lake Taupo expose transgressive sequences that range from beach face deposits at the base to below-storm wave-base deposits at the top. Many terraces are capped by deposits of well-rounded, cobble- to boulder-size pumice clasts, which are interpreted as stranded deposits of previously floating clasts, formed during rapid lake-level fall. The Lake Taupo sedimentary record provides insights into sedimentary facies and styles that may be expected during lake filling that immediately follows caldera collapse. The inferred rapid filling rate of the lake, estimated to be 5-9 m yr-1 for the exposed section, together with the dominantly vitric nature of the source material, permitted preservation and recognition of deposits such as shoreface storm-wave deposits that are unusual in non-volcaniclastic lake settings.

Original languageEnglish (US)
Title of host publicationVolcaniclastic Sedimentation in Lacustrine Settings
PublisherWiley-Blackwell Publishing Ltd
Pages151-177
Number of pages27
ISBN (Print)9781444304251, 0632058471, 9780632058471
DOIs
StatePublished - Mar 24 2009

Fingerprint

wave energy
sedimentation
lake
sediment
ignimbrite
caldera
energy
pumice
lake level
clast
detritus
terrace
shoreline
dam
effect
shore (nonmarine)
wave action
highstand
boulder
lacustrine deposit

Keywords

  • High energy and low sediment influx - Waipehi and Kaiapo Bay
  • High-energy and high sediment-influx rate - Five Mile Beach
  • Lake Taupo sedimentation
  • Low energy and high sediment influx rate - Waitahanui, Kuratau and Poukura Pa
  • Low-energy and low sediment-influx rate - Kinloch, Hingapo and Acacia Bay
  • Post-1.8-ka marginal sedimentation in Lake Taupo, New Zealand - effects of wave energy and sediment supply in a rapidly rising lake
  • Sedimentation patterns - transgressive surface, wave energy, typical deepening succession and lake draining
  • Taupo volcano and lake Taupo deposits - offshore deposits, shoreface deposits, shoreline deposits
  • The homogeneity of lithofacies - due to rapid lake rise and burial of accumulating deposits
  • Variations in lithofacies associations around Lake Taupo

ASJC Scopus subject areas

  • Earth and Planetary Sciences(all)

Cite this

Riggs, N. R., Ort, M. H., White, J. D. L., Wilson, C. J. N., Houghton, B. F., & Clarkson, R. (2009). Post-1.8-ka Marginal Sedimentation in Lake Taupo, New Zealand: Effects of Wave Energy and Sediment Supply in a Rapidly Rising Lake. In Volcaniclastic Sedimentation in Lacustrine Settings (pp. 151-177). Wiley-Blackwell Publishing Ltd. https://doi.org/10.1002/9781444304251.ch8

Post-1.8-ka Marginal Sedimentation in Lake Taupo, New Zealand : Effects of Wave Energy and Sediment Supply in a Rapidly Rising Lake. / Riggs, Nancy R; Ort, Michael H; White, J. D L; Wilson, C. J N; Houghton, B. F.; Clarkson, R.

Volcaniclastic Sedimentation in Lacustrine Settings. Wiley-Blackwell Publishing Ltd, 2009. p. 151-177.

Research output: Chapter in Book/Report/Conference proceedingChapter

Riggs, NR, Ort, MH, White, JDL, Wilson, CJN, Houghton, BF & Clarkson, R 2009, Post-1.8-ka Marginal Sedimentation in Lake Taupo, New Zealand: Effects of Wave Energy and Sediment Supply in a Rapidly Rising Lake. in Volcaniclastic Sedimentation in Lacustrine Settings. Wiley-Blackwell Publishing Ltd, pp. 151-177. https://doi.org/10.1002/9781444304251.ch8
Riggs NR, Ort MH, White JDL, Wilson CJN, Houghton BF, Clarkson R. Post-1.8-ka Marginal Sedimentation in Lake Taupo, New Zealand: Effects of Wave Energy and Sediment Supply in a Rapidly Rising Lake. In Volcaniclastic Sedimentation in Lacustrine Settings. Wiley-Blackwell Publishing Ltd. 2009. p. 151-177 https://doi.org/10.1002/9781444304251.ch8
Riggs, Nancy R ; Ort, Michael H ; White, J. D L ; Wilson, C. J N ; Houghton, B. F. ; Clarkson, R. / Post-1.8-ka Marginal Sedimentation in Lake Taupo, New Zealand : Effects of Wave Energy and Sediment Supply in a Rapidly Rising Lake. Volcaniclastic Sedimentation in Lacustrine Settings. Wiley-Blackwell Publishing Ltd, 2009. pp. 151-177
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AB - The eruption of Taupo caldera, New Zealand, c. 1.8 ka, climaxed in the emplacement of the Taupo ignimbrite, which dammed the previous outlet of the caldera lake and allowed rise of the lake behind the dam to c. 34 m above current lake level. After an estimated 20 yrs of lake refilling, the ignimbrite dam was breached, and the lake drained rapidly to a position 2-4 m above current level. From that level, the lake apparently dropped slowly to its present position. Post-1.8-ka lacustrine sediments are exposed at various levels between the highstand and the modern shoreline. The distribution of lacustrine facies at Taupo reflects the location of the mouths of rivers that drained uplands buried and/or denuded of vegetation by the erupted material, together with the position of depositional sites with respect to prevailing winds and energy systems. Four broad facies environments can be recognized, defined by combinations of high or low energy and high or low sediment influx. Sediments deposited in areas of high energy (i.e. strong wave action) and high sediment input are rich in vitric material, but contain abundant lithic material in those deposits interpreted as storm influenced. Deposits in low-energy areas that had high sediment input are dominantly vitric, with abundant shoreface and pumice-raft deposits. High-energy, low-sediment-input areas are rich in lithic detritus, apparently reworked from ignimbrites along the pre-eruptive lake shore during storms. Deposits that characterize low-energy, low-sediment-input environments are poor in lithic detritus, reflecting the inability of currents to transport material to these sites. Terraces prominent above the modern shoreline of Lake Taupo expose transgressive sequences that range from beach face deposits at the base to below-storm wave-base deposits at the top. Many terraces are capped by deposits of well-rounded, cobble- to boulder-size pumice clasts, which are interpreted as stranded deposits of previously floating clasts, formed during rapid lake-level fall. The Lake Taupo sedimentary record provides insights into sedimentary facies and styles that may be expected during lake filling that immediately follows caldera collapse. The inferred rapid filling rate of the lake, estimated to be 5-9 m yr-1 for the exposed section, together with the dominantly vitric nature of the source material, permitted preservation and recognition of deposits such as shoreface storm-wave deposits that are unusual in non-volcaniclastic lake settings.

KW - High energy and low sediment influx - Waipehi and Kaiapo Bay

KW - High-energy and high sediment-influx rate - Five Mile Beach

KW - Lake Taupo sedimentation

KW - Low energy and high sediment influx rate - Waitahanui, Kuratau and Poukura Pa

KW - Low-energy and low sediment-influx rate - Kinloch, Hingapo and Acacia Bay

KW - Post-1.8-ka marginal sedimentation in Lake Taupo, New Zealand - effects of wave energy and sediment supply in a rapidly rising lake

KW - Sedimentation patterns - transgressive surface, wave energy, typical deepening succession and lake draining

KW - Taupo volcano and lake Taupo deposits - offshore deposits, shoreface deposits, shoreline deposits

KW - The homogeneity of lithofacies - due to rapid lake rise and burial of accumulating deposits

KW - Variations in lithofacies associations around Lake Taupo

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