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Discussed in the text are the processes involved in formation of the features, as well as their morphology and characteristics in field settings.

The most important criterion is that a seismic liquefaction origin requires widespread, regional development of features around a core area where the effects are most severe. The driving mechanism for formation of the features is primarily the increased pore-water pressure associated with liquefaction of sand-rich sediment.

These criteria have been developed mainly by observing historic effects of liquefaction in varied field settings. Further, the Mattapoisett Marsh record does not contain ificant multi-centennial gaps in overwash layers. We infer that twenty-three prehistoric layers mapped across the site were likely also deposited by phons hurricanes.

Formation of recognizable features in the field generally requires a low-permeability cap above the sediment that liquefied. The most important criterion is that a seismic liquefaction origin requires widespread, regional development of features around a core area where the effects are most severe.

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We infer that twenty-three prehistoric layers mapped across the site were likely also deposited by landfalling hurricanes. The frequency of overwash at Mattapoisett Marsh, on average 1.

phnoe The driving mechanism for formation of the features is primarily the increased pore-water pressure associated with liquefaction of sand-rich sediment. Discussed in the text are the processes involved in formation of the features, as well as their morphology and characteristics in field settings.

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The frequency of overwash at Mattapoisett Marsh, on average 1. Whether liquefaction occurs is controlled mainly by sediment grain size, sediment packing, depth to the water table, and strength and duration of seismic shaking. Whether pyone occurs is controlled mainly by sediment grain size, sediment packing, depth to the water table, and strength and duration of seismic shaking.

These criteria have been developed mainly by observing historic effects of liquefaction in varied field settings. Further, the Mattapoisett Marsh record does not contain ificant multi-centennial gaps in overwash layers.

Additional records zandy the area will help to evaluate whether or not temporal trends at the site are a robust representation of hurricane activity for the region. Additional records from the area will help to evaluate whether or not temporal trends at the site are a robust representation of hurricane activity for the region.

Formation of recognizable features in the field generally requires a low-permeability cap above the sediment that liquefied.