The size and shape of these linear features resemble those of gutter casts of sand protruding into shale in other deposits.
Gutter marks geology.
Tool marks also have a more specific breakdown.
A dictionary of earth sciences.
Two thin sandstone and siltstone horizons in the middle lias lower jurassic of the yorkshire coast informally called the lower and upper striped beds are characterised by small scale fining upward layers associated with filled scour channels gutter marks.
Gutter casts can be especially useful for the interpretation of storm deposits and facies trends in shallow marine carbonate environments.
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Gutter cast in the bencliff grit osmington mills dorset.
For more on gutter marks or gutter casts or scour and fill see.
The gravel filled gutter casts of the merced formation show a strongly preferred east to northeast orientation approximately normal to the shoreline trend inferred on the basis of the modern shoreline trend and the regional structural grain.
Groove or striation marks result from the continuous contact with the muddy bed.
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These represent the casts of small scale erosional channels cut into consolidated mud.
The overlying bed may be a small fraction of the thickness of the gutter cast to several times its thickness or in cases the gutter casts are isolated scour fills surrounded by mudstone or shale.
There are grooves and striations skip or prod marks and roll marks.
The gutters are up to 5 m long 50 500 mm wide and up to 200 mm deep and have variable cross sections.
The term gutter marks applies to the initial troughs cut into the muddy floor of the depositional basin but these original structures like flute and groove marks are unlikely to be preserved.
Gutter casts have been in terpreted to occupy areas domi nated by sediment bypass across which high velocity sediment laden flows eroded deep n arrow scours gutters into a muddy substrate.
This support fitting is designed with seals and fitting marks that indicate that correct gutter placement to allow for expansion and contraction.
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Skip or prod marks come from objects that bounce along the surface of the muddy bed.
The striping and associated sedimentary sinuous narrow channel like features known as gutter marks have been described by greensmith rawson and shalaby 1980.
The iithology of the gutter mark infillings is either dominantly calcareous consisting of laminated calcareous siltstone or bioclastic limestone or else.