shernren
you are not reading this.
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By "route" I mean the entire surface of the Lewis Overthrust.
Montana is 600+ miles long. Its entire northern belt is disturbed. The Lewis Overthrust is by your own estimate 40-130 miles long. For a 40-130-mile-long structure to disturb an entire belt roughly 600 miles long sounds like enough damage to me. Now can you show me a single place along the Lewis Overthrust where there is evidence that no grinding occurred?
laptoppop said:But let me ask you then -- how DID the layers form? How are critters encapsulated so that they fossilize and not decay?
I believe the question is between local and global floods, not between floods and ???? With a local flood you have an additional problem -- that of dissolving the material in question sufficiently to make the deposits.
Long-term deposition would not result in fossils, and would not explain the purity of separation either.
No way! Laptoppop, did you forget everything that transpired around post #26. Do you want me to go through that again?
Ediacara: Deep turbidite and shallow slow deposition.
Maotianshan: Shallow sea with muddy bottom.
Emu Bay: Shallow water deposition.
Sirius Passet: Deep-sea deposition.
House Range: Deep-sea sediments punctuated by landslides.
Burgess Shale: Ditto.
Orsten: Anoxic deep-sea shore.
Soom Shale: Laminated silts and muds atop tillite.
Wenlock series: Fine-grained marine muds interspersed with ash.
Rhynie Chert: Rising of silica-rich water (volcanic associations) causing instant petrification.
Hunsruck Slates: Rapid burial in sediments with low organic content.
Canowindra: Drying out of a lake.
Bear Gulch Limestone: Fossilization during anoxic intervals interspersed with worm burrows during non-anoxic intervals, in arid climate (gypsum formation).
Mazon Creek: Rapid sedimentary burial with siderite concretions.
Hamilton Quarry: Interbedded laminated mudstones and limestones.
Ghost Ranch: Flood hurls Coelophysis into pool and kills them.
La-Voulte-Sur-Rhone: Low energy marine basin.
Solnhofen: Salinity stratification due to high evaporation rates.
Yixian: Still lake sediments punctuated by volcanic ash.
Santana and Crato: widely varying sediments separated by evaporites.
Xiagou: Tranquil lake deposition with varves.
Auca Mahuevo: Undisturbed floodplains.
Green River Formation: Varves!
Monte Bolca: Mudstone with well-preserved fossils interspersed by less rich limestones.
Messel Pit: Lake deposition with extreme stratification leading to extremely anoxic bottom conditions.
London Clay: Inconclusive.
That, laptoppop, is how fossils are formed - anoxic preservation. Whoever told you that geologists frequently attribute fossils to flooding was lying to you. (I hate having to use such a strong word but I'm not holding back any punches.) Geologists know what flooding looks like and know when to attribute fossils to it, as in the case of the Hunsruck Slates and Ghost Ranch. But they know how to look for signs of a flood and know when the signs of a flood are not there, and then can find signs of alternative mechanisms to attribute it to.
Fossil deposition does not require floods of any kind!
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