to verify and compare parameters for headland systems in
the future as sites continue to mature.
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Cross-references
Coastal Erosion Control
Shore Protection
Tombolo
HEAVY MINERALS
Ilya V. Buynevich
Department of Earth and Environmental Science,
College of Science and Technology, Temple University,
Philadelphia, PA, USA
Definition
Heavy minerals refer to minerals with density >2.9 g/cm
3
.
Description
In addition to their use as sediment source (provenance)
indicators, heavy minerals (garnet, magnetite, ilmenite,
tourmaline, zircon, hornblende, etc.) provide important
information about hydrodynamic conditions responsible
for erosion and deposition of estuarine sediments
(Komar, 2007). Increases in transport energy due to
floods, storms, or tsunamis often generate diagnostic
heavy-mineral
concentrations
(HMCs)
through
a combination of selective sorting factors that result from
differences between the light (quartz, feldspar, muscovite,
calcite) and heavy-mineral fraction (Figure 1).
On shorter timescales, tidal flow regime and wavegenerated flows may produce localized enrichment in
heavy-mineral components. Estuarine bedforms, such as
two- and three-dimensional ripples and megaripples,
may cause preferential accumulation of denser minerals
along their crests. In some regions of tidal channels,
estuarine beaches, and adjacent dune fields, prolonged
selective sorting may result in economically viable
concentrations (placers). HMCs containing magnetite
provide distinct magnetic susceptibility signatures in estuarine sequences making them valuable event indicators.
When analyzing siliciclastic estuarine deposits, HMC
thickness, concentration factor, granulometry, and spatial
distribution should provide valuable information about
past estuarine dynamics.
HEAVY MINERALS
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