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Dish
Structures. This image shows what can be considered
the early stages of the development of dish
structures. The muddy laminae have become irregular
and some are beginning to break apart, but well-developed
dish structures have not formed. The image below
shows the structure that develops when dewatering
proceeds further than it has in this example. |
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Dish and
Pillar Structures. This image shows well-developed
stuctures. The presence of dish structures are
evidence of rapid sediment deposition. They form by
the escape of water during consolidation of the sediment.
The initial bed consists of sand interbedded with
thin, lesser-permeability mud laminae. As fluids
move upward during compaction and dewatering, they are
impeded by the muddy laminae, causing them to travel
horizontally until an easier path for escape is
encountered. The muddy laminae create the convex-up
dishes, while the pillars serve as the fluid escape
paths. |
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Dish
Structures. Note the convex-up dish structures
scattered across this outcrop. These structures are
not as pronounced as in the above image, perhaps because
compaction and dewatering has proceeded to such an extent
that some of the previously formed structures have become
deformed. |
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Fluid Escape
Pipes. These structures form in a similar fashion
to dish structures with the exception that the original
sediment was probably more homogeneous and lacked a
significant muddy component. As fluids dewatered,
the escape paths were preserved as vertical pipes, seen
here. When you see vertical structures like these, you've
got to be careful not to confuse them with vertical
burrowssome organisms, particularly Skolithos,
create features that are strikingly similar. |