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Interpretations	  of	  high-­‐resolution	  geophysical	  data	  and	  analysis	  of	  the physical	  properties	  of	  vibracores	  from	  separate,	  but	  closely	  related	  study	  sites have	  contributed	  to	  our	  understanding	  of	  the	  Late	  Quaternary paleoenvironments	  of	  southern	  New	  England.	  	  Two	  submerged	  areas,	  Cedar	  Tree Beach	  located	  in	  the	  northwest	  corner	  of	  Greenwich	  Bay	  and	  the	  Mud	  Hole,	  a deep	  bathymetric	  depression	  located	  at	  the	  southern	  edge	  of	  the	  Rhode	  Island Sound	  have	  been	  designated	  as	  study	  sites	  for	  the	  Bureau	  of	  Ocean	  Energy Management	  (BOEM)	  Paleocultural	  study,	  which	  seeks	  to	  develop	  best	  practices methodology	  when	  developing	  the	  continental	  shelf	  for	  renewable	  energy projects.	  	  Reconstructions	  of	  a	  post-­‐glacial,	  pre-­‐marine	  inundation paleoenvironment	  is	  a	  critical	  step	  in	  the	  development	  of	  an	  archaeological predictive	  model	  to	  better	  understand	  potential	  for	  habitability	  and	  preservation of	  cultural	  material. The	  first	  chapter	  is	  focused	  on	  interpreting	  post-­‐glacial	  depositional environments	  of	  the	  Mud	  Hole	  study	  area.	  	  High-­‐resolution	  geophysical	  data consisting	  of	  37	  survey	  lines	  with	  500	  m	  spacing	  and	  covering	  ~130	  km2 including	  CHIRP	  seismic	  reflection	  and	  interferometric	  side-­‐scan	  and	  swath bathymetry	  data	  were	  collected	  in	  2012.	  	  Side-­‐scan	  imagery	  was	  inspected	  for sedimentary	  features.	  	  Megaripples	  were	  interpreted	  as	  areas	  of	  modern sediment	  reworking	  due	  to	  storm-­‐induced	  bottom	  currents.	  	  Erosional	  outliers and	  scour	  depressions	  were	  interpreted	  as	  net-­‐erosional	  sedimentary

Reconstructing Submerged Paleoenvironments: Mud Hole, RI Sound and Greenwich Bay, RI