Geophysical Visualization of Reef Island Accretion and Stratigraphic Architecture using Ground Penetrating Radar

Liang, Yiqing, Kench, Paul S., Ford, Murray R. and East, Holly (2019) Geophysical Visualization of Reef Island Accretion and Stratigraphic Architecture using Ground Penetrating Radar. In: Coastal Sediments 2019: Advancing Science & Engineering for Resilient Coastal Systems, 27th - 31st May 2019, St. Petersburg, USA.

Full text not available from this repository.
Official URL: http://dx.doi.org/10.1142/9789811204487_0160

Abstract

Coral reef islands are small, low-lying landforms that provide the only habitable land for atoll nations and support a range of endemic flora and fauna. Thus, the vulnerability of these islands to projected sea-level rise is a global concern. The internal structure and modes of island accretion are integral in understanding how islands have formed and subsequently, how they will change in the future. This study employs extensive ground penetrating radar (GPR) imaging on a reef island on Huvadhoo Atoll, Maldives, combined with island coring and stratigraphic analyses, in order to infer styles of island accretion. The GPR images imply central core accretion, with vertical accretion occurring on the initial core and progradation occurring outwards in both directions. However, some transects display progradation occurring predominately in one direction, which may also indicate erosional and rollover or overwash processes that could have led to island migration. Furthermore, using inferences of major radar units and boundary changes in signal reflectors combined with detailed subsurface sedimentology, the subsurface stratigraphy of the island sediments was divided into four discrete facies: velu (lagoon infill), finolhu (initial island core), athiri (beach and paleobeach), and muraka (surface layer) facies. The GPR records on KAN provide visual evidence of the mode of island evolution to complement previous theoretical interpretations, and have demonstrated the capability of GPR to discern sedimentary facies, subsurface features, and changes in sediment characteristics on reef islands. Results from this study show past processes of island building and could infer island response to various stages of sea-level change, which has implications for the stability of reef islands in the face of projected sea-level rise.

Item Type: Conference or Workshop Item (Paper)
Subjects: F800 Physical and Terrestrial Geographical and Environmental Sciences
Department: Faculties > Engineering and Environment > Geography and Environmental Sciences
Depositing User: Paul Burns
Date Deposited: 20 Jun 2019 09:56
Last Modified: 10 Oct 2019 17:47
URI: http://nrl.northumbria.ac.uk/id/eprint/39742

Actions (login required)

View Item View Item

Downloads

Downloads per month over past year

View more statistics


Policies: NRL Policies | NRL University Deposit Policy | NRL Deposit Licence