Follets Island

A case of unprecedented change and transition from rollover to subaqueous shoals

Christopher I. Odezulu, Jorge Lorenzo Trueba, Davin J. Wallace, John B. Anderson

Research output: Chapter in Book/Report/Conference proceedingChapterResearchpeer-review

10 Citations (Scopus)

Abstract

Follets Island, a transgressive island located on the upper Texas coast, is an ideal location to study barrier island transition from a rollover subaerial barrier to subaqueous shoals. This system also allows for an examination of coastal response to accelerated sea-level rise, storms, and sediment supply. The landward shoreline retreat rate during historical time is similar to the landward retreat rate of the bay shoreline, hence its current classification as a rollover barrier. However, the island has a limited and diminishing sand supply, which makes it even more vulnerable to erosion during storms and relative sea-level rise. Four core transects that extend from the upper shoreface to the back barrier bay are used to constrain the thickness of washover, barrier and upper shoreface deposits and to estimate sediment fluxes in the context of the overall sand budget for the island over centennial timescales. Stratigraphic architecture reveals two prominent transgressive surfaces. A lower flooding surface separates red fluvial-deltaic clay from overlying bay mud and an upper erosional surface separates back-barrier deposits from overlying shoreface and foreshore deposits. Radiocarbon ages are used to constrain the evolution of the barrier and its long-term rate of island migration whereas 210Pb dates are used to constrain the modern sand overwash flux. Results show that significant washover sands are deposited in the bay and about twice this volume is deposited as subaerial washover deposits. The total sand washover volume shows that overwash processes account for about half of the sand produced by shoreline erosion in historical time. Our results also indicate that the historical rate of shoreline retreat is about an order of magnitude faster than the geologic rate. We estimate back-barrier accommodation space to be about three times greater than the volume of the barrier. Hence, given the current shoreline erosion and overwash flux rate, Follets Island will eventually transition from a subaerial rollover barrier to subaqueous shoals. The frequency of severe storms along the Texas coast is not believed to have varied significantly in recent time, but the rate of sea-level rise has increased approximately five-fold and sand supply to the island is minimal. This leads us to suggest that accelerated sea-level rise and diminished sand supply are the main causes of this unprecedented change.

Original languageEnglish
Title of host publicationBarrier Dynamics and Response to Changing Climate
PublisherSpringer International Publishing
Pages147-174
Number of pages28
ISBN (Electronic)9783319680866
ISBN (Print)9783319680842
DOIs
StatePublished - 15 Feb 2018

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Islands
Oceans and Seas
Budgets

Keywords

  • Antecedent topography
  • Coastal erosion
  • Flooding surface
  • Numerical modeling
  • Overwash
  • Rollover
  • Sea level
  • Sediment flux
  • Texas coast
  • Transgressive barrier

Cite this

Odezulu, C. I., Lorenzo Trueba, J., Wallace, D. J., & Anderson, J. B. (2018). Follets Island: A case of unprecedented change and transition from rollover to subaqueous shoals. In Barrier Dynamics and Response to Changing Climate (pp. 147-174). Springer International Publishing. https://doi.org/10.1007/978-3-319-68086-6_5
Odezulu, Christopher I. ; Lorenzo Trueba, Jorge ; Wallace, Davin J. ; Anderson, John B. / Follets Island : A case of unprecedented change and transition from rollover to subaqueous shoals. Barrier Dynamics and Response to Changing Climate. Springer International Publishing, 2018. pp. 147-174
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Odezulu, CI, Lorenzo Trueba, J, Wallace, DJ & Anderson, JB 2018, Follets Island: A case of unprecedented change and transition from rollover to subaqueous shoals. in Barrier Dynamics and Response to Changing Climate. Springer International Publishing, pp. 147-174. https://doi.org/10.1007/978-3-319-68086-6_5

Follets Island : A case of unprecedented change and transition from rollover to subaqueous shoals. / Odezulu, Christopher I.; Lorenzo Trueba, Jorge; Wallace, Davin J.; Anderson, John B.

Barrier Dynamics and Response to Changing Climate. Springer International Publishing, 2018. p. 147-174.

Research output: Chapter in Book/Report/Conference proceedingChapterResearchpeer-review

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AU - Wallace, Davin J.

AU - Anderson, John B.

PY - 2018/2/15

Y1 - 2018/2/15

N2 - Follets Island, a transgressive island located on the upper Texas coast, is an ideal location to study barrier island transition from a rollover subaerial barrier to subaqueous shoals. This system also allows for an examination of coastal response to accelerated sea-level rise, storms, and sediment supply. The landward shoreline retreat rate during historical time is similar to the landward retreat rate of the bay shoreline, hence its current classification as a rollover barrier. However, the island has a limited and diminishing sand supply, which makes it even more vulnerable to erosion during storms and relative sea-level rise. Four core transects that extend from the upper shoreface to the back barrier bay are used to constrain the thickness of washover, barrier and upper shoreface deposits and to estimate sediment fluxes in the context of the overall sand budget for the island over centennial timescales. Stratigraphic architecture reveals two prominent transgressive surfaces. A lower flooding surface separates red fluvial-deltaic clay from overlying bay mud and an upper erosional surface separates back-barrier deposits from overlying shoreface and foreshore deposits. Radiocarbon ages are used to constrain the evolution of the barrier and its long-term rate of island migration whereas 210Pb dates are used to constrain the modern sand overwash flux. Results show that significant washover sands are deposited in the bay and about twice this volume is deposited as subaerial washover deposits. The total sand washover volume shows that overwash processes account for about half of the sand produced by shoreline erosion in historical time. Our results also indicate that the historical rate of shoreline retreat is about an order of magnitude faster than the geologic rate. We estimate back-barrier accommodation space to be about three times greater than the volume of the barrier. Hence, given the current shoreline erosion and overwash flux rate, Follets Island will eventually transition from a subaerial rollover barrier to subaqueous shoals. The frequency of severe storms along the Texas coast is not believed to have varied significantly in recent time, but the rate of sea-level rise has increased approximately five-fold and sand supply to the island is minimal. This leads us to suggest that accelerated sea-level rise and diminished sand supply are the main causes of this unprecedented change.

AB - Follets Island, a transgressive island located on the upper Texas coast, is an ideal location to study barrier island transition from a rollover subaerial barrier to subaqueous shoals. This system also allows for an examination of coastal response to accelerated sea-level rise, storms, and sediment supply. The landward shoreline retreat rate during historical time is similar to the landward retreat rate of the bay shoreline, hence its current classification as a rollover barrier. However, the island has a limited and diminishing sand supply, which makes it even more vulnerable to erosion during storms and relative sea-level rise. Four core transects that extend from the upper shoreface to the back barrier bay are used to constrain the thickness of washover, barrier and upper shoreface deposits and to estimate sediment fluxes in the context of the overall sand budget for the island over centennial timescales. Stratigraphic architecture reveals two prominent transgressive surfaces. A lower flooding surface separates red fluvial-deltaic clay from overlying bay mud and an upper erosional surface separates back-barrier deposits from overlying shoreface and foreshore deposits. Radiocarbon ages are used to constrain the evolution of the barrier and its long-term rate of island migration whereas 210Pb dates are used to constrain the modern sand overwash flux. Results show that significant washover sands are deposited in the bay and about twice this volume is deposited as subaerial washover deposits. The total sand washover volume shows that overwash processes account for about half of the sand produced by shoreline erosion in historical time. Our results also indicate that the historical rate of shoreline retreat is about an order of magnitude faster than the geologic rate. We estimate back-barrier accommodation space to be about three times greater than the volume of the barrier. Hence, given the current shoreline erosion and overwash flux rate, Follets Island will eventually transition from a subaerial rollover barrier to subaqueous shoals. The frequency of severe storms along the Texas coast is not believed to have varied significantly in recent time, but the rate of sea-level rise has increased approximately five-fold and sand supply to the island is minimal. This leads us to suggest that accelerated sea-level rise and diminished sand supply are the main causes of this unprecedented change.

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KW - Coastal erosion

KW - Flooding surface

KW - Numerical modeling

KW - Overwash

KW - Rollover

KW - Sea level

KW - Sediment flux

KW - Texas coast

KW - Transgressive barrier

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BT - Barrier Dynamics and Response to Changing Climate

PB - Springer International Publishing

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Odezulu CI, Lorenzo Trueba J, Wallace DJ, Anderson JB. Follets Island: A case of unprecedented change and transition from rollover to subaqueous shoals. In Barrier Dynamics and Response to Changing Climate. Springer International Publishing. 2018. p. 147-174 https://doi.org/10.1007/978-3-319-68086-6_5