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- Newsgroups: talk.origins
- Path: sparky!uunet!nntp1.radiomail.net!fernwood!aurora!isaak
- From: isaak@aurora.com (Mark Isaak)
- Subject: Response to the Response to the Flood FAQ
- Message-ID: <1992Dec30.170525.6031@aurora.com>
- Reply-To: isaak@aurora.com (Mark Isaak)
- Organization: The Aurora Group, Palo Alto, CA
- Date: Wed, 30 Dec 92 17:05:25 GMT
- Lines: 248
-
-
- [The following is from Andrew MacRae (macrae@pandora.geo.ucalgary.ca),
- who cannot post himself.]
-
- Response to the response to the Flood FAQ, part 1
-
- 1. MOUNTAINS AND SEDIMENTATION RATES
- > Wayne Folta
- >> isaak@aurora.com (Mark Isaak)
- >> How were mountains formed? Many very tall mountains are composed of
- >> sedimentary rocks. If these were laid down during the flood, how
- >> did they reach their present height, and when were the valleys
- >> between them eroded away?
-
- >As the land was raised up and the flood waters settled down into the ocean
- >basins, mountains would be raised and great erosion would occur.
-
- But what was the mechanism for "the land was raised up", and how is
- it distinguished from the conventional, tectonic explanation?
- Also, 1) flood up - deposit sediments with marine fossils
- 2) flood down - raise mountains, erode valleys
- Where did the sediments deposited in 1) erode from, since most of
- the flood erosion apparently occurred during 2)? You need something high to
- erode to produce the sediments. Sediments do not appear from nowhere.
-
- >(This reminds me of the Mt. St. Helens video that Gish and company have.
- >It shows a valley with a little stream running through it. The valley's
- >walls show millions of fine layers of deposits. Three hundred years from
- >now, people might assume that the layers had been deposited over millions
- >of years and that the stream had taken hundreds of thousands of years to
- >carve out the valley. In fact, the deposits occured in three days, and the
- >valley was blown out by a huge steam/mud flood in half a day.)
-
- Wow! Since you are dealing with a very high relief landscape with
- little vegetation (a volcanic mountain), of course erosion rates are high.
- I or any other geologist would _NOT_ assume the layers had been deposited
- over millions of years, because volcanic terraines are _always_ areas of
- high depositional and erosional rates, dominated by catastrophic events
- (this is probably why creation "scientists" study modern environments there
- :-). Such events (e.g., debris flows, pyroclastic fallout deposits, surge
- deposits, etc.) produce sedimentary structures quite distinct from slower
- sedimentary processes. It would be blatently obvious that the rock with the
- "millions of fine layers" was volcanic in origin, especially if you looked
- at the rock in thin section under the microscope.
-
- Unfortunately for flood hypotheses, volcanic environments are very
- distinctive, and make up a small part of depositional environments preserved
- in the rock record. Most of the environments preserved in the many
- kilometres of sediment found in depositional basins is ocean bottom or
- deltaic. Do Morris et al. have a movie of the catastophic depositional
- rates and erosion rates on the Mississippi Delta? Sure, there are levee
- breaches, but these are relatively infrequent, and quite small in scope
- compared to the size of the entire delta complex. Most of the deposition is
- slow, at least in a vertical sense, because there are only a few metres of
- accomodation between the sediment bottom and sea level. You can deposit a
- few metres of sediment to infill a bay, but once you are at sea-level,
- deposition almost stops, because there is no "hole" to fill.
-
- The Mississippi Delta complex has >5 km of sediment beneath it, deposited
- over thousands of square kilometres. Even if it was possible to deposit
- huge volumes of mud overnight as at Mt. St. Helens, it would still take
- thousands of years to equal the volume of sediment in the Mississippi Delta
- basin alone. Gosh, you could probably take _all_ the volume of Mt. St.
- Helens, and it would still take thousands of equivalent volumes to fill the
- basin. However, it isn't possible to deposit at the huge Mt. St. Helens
- rates anyway, since you would change the structure of the delta sediments
- completely (no fine bedding, wave ripples, coal beds, oyster beds, in-place
- tree stumps, paleosols (fossil soils), etc.).
-
- Another strange problem of the flood model is how trees and other land
- plants can form coal in areas that are now well below sea level. Did the
- flood waters also drop a kilometre below the current sea level so dry land
- could form? (The conventional explanation is that the weight of the
- overlying sediments has caused the terrestrial sediments to subside well
- below sea level after deposition). I know, Morris et al. may have some
- magical, catastophic explanation for coal; that claims it isn't composed of
- terrestrial plants, or they claim that the plants accumulated in huge mats
- of material during the flood. Funny how the plants still managed to sort
- themselves into stratigraphically distinct coal types (giant lycopod coals
- in the Carboniferous, cypress coals in the Cretaceous, etc.).
-
- >In Whitcomb and Morris, they speculate that the water level fell, on
- >average, at 15 feet per day.
-
- Wow! What an incredible rate of fall! That water must have torn
- into solid bedrock, excavating valleys thousands of metres deep and
- producing thousands of cubic kilometres of sediment from solid rock - NOT!
- Even if you scraped up _all_ the loose sediment now on the surface of the
- Earth now, it would be a tiny fraction of the amount in the 10+ km deep
- sedimentary basins of the world. So you have to produce the sediment from
- the bedrock - somehow. I don't care how violent the flood was - you can not
- turn granite into cubic kilometres of clay in a short amount of time. The
- process is limited by chemical reactions that are controlled by physics.
-
- According you the rate you quote, the rate of fall of the flood was
- _less_ violent that the daily tidal flux in the Bay of Fundy, Nova Scotia,
- which varies on the order of 15 _metres_ twice per day. Wow.
- What a cataclysm :-)
-
- If Whitcomb and Morris are claiming a rate of 15 feet per day, they
- must have some evidence of how long it took for the water to fall. How long
- do they say there is to erode km deep valleys into _bedrock_ (not the
- unconsolidated sediments on Mt. St. Helens flanks)?
-
-
- 2. ANGULAR AND OTHER UNCONFORMITIES
-
- >> How does a global flood explain angular unconformities, where one set
- >> of layers of sediments have been extensively modified (e.g., tilted)
- >> and eroded before a second set of layers were deposited on top?
- >> They thus seem to require at least two periods of deposition (more,
- >> where there is more than one unconformity) with long periods of
- >> time in between.
-
- >Why long periods in between?
-
- Why long:
- 1) Evidence for chemical weathering at the surface (i.e. chemical
- alteration of the underlying rocks). Often paleosols (fossil soils) are
- present. The chemistry of the alteration process implies a long time (how
- long does it take for a soil to form from bare bedrock?).
- 2) _Rounded_ pebbles composed of the underlying rock deposited in
- the overlying units. Rounding in streams takes time.
- 3) You must tilt the underlying rocks before (or while) eroding
- them, then deposit near horizontal beds on top. The deformation to produce
- the tilting (i.e. mountain building) takes time, and must occur before
- depositing the overlying units.
- 4) Many angular unconformities are on top of igneous intrusive rocks
- (e.g., granite) that imply a great deal of time because: A) the igneous rock
- must be intruded kilometres below the surface (the kinematics of the
- crystals in the rock constrain the pressure), B) they must cool slowly to
- produce large crystals (calculate how long it takes many cubic kilometres of
- rock at 600+ degrees Celcius to cool), C) then you must erode the kilometres
- of rock off the top of the intrusive, _and_ D) erode the intrusive igneous
- rock so you can deposit pebbles in the sediments overlying the unconformity.
- This is observed at _many_ localities worldwide, of _different_ ages (see
- below for an example).
-
- >Does this assume that deposits made during the
- >Flood would be from settling silt?
-
- No. Any sedimentary rock. An "angular" unconformity implies an
- episode of deformation _before_ the erosion to produce the tilted beds; but
- general unconformities can have any geometry. The underlying rocks at an
- unconformity do not have to be sedimentary on both sides. The point is that
- you have an older structure in the underlying rock that is cut by a younger
- structure - the erosion surface or unconformity. The unconformity divides
- two sets of events - before the erosion, and after. This is termed a
- "cross-cutting" relationship, and is one of the principles of geology - the
- structures that are "cut" are older than the structures doing the cutting
- (in this case the erosion surface or unconformity). You can't, for
- instance, make the erosion surface first, then intrude the granite and put
- pebbles of it in the overlying rocks. It could not occur in this backwards
- fashion.
- Do you see why finding unconformities causes problems for a
- single-event flood? There are plenty of unconformities in the rock record.
- Every one of them implies 1 period of deposition before the unconformity, 1
- period of erosion (sometimes subaerial), and 1 period of renewed deposition.
- In the case of _angular_ unconformities, you must also fit a period of
- deformation before the renewed deposition.
- Surely you can see that this would imply multiple "floods", or a
- greatly complicated "flood history" that is at odds with the models "flood
- creationists" have proposed.
-
- >Surely deposits could be made by moving
- >vast amounts of land much more quickly than that?
-
- You can create the geometry of an angular unconformity (intersecting
- beds), but you will not find pebbles of the underlying rocks in the
- overlying ones - and yes, this situation (incorporation of pebbles into the
- overlying units) is very common.
-
- >And how about the Colorado Plateau (Whitcomb & Morris, pg. 160), which
- >occupies 250,000 square miles, and which has been uplifted multiple times
- >(this believed because of disconformities in the stratigraphic sequences)
- >and yet is nearly perfectly flat? This causes a problem for non-Flood
- >geologies.
-
- Actually, the Coldoro Plateau is _relatively_ flat, but it it far
- from "perfectly flat" or undeformed. For instance, there are broad
- structural domes and faulting in the vicinity of Moab and Canyonlands
- National Park. The Coldorado Plateau is cut by the Rio Grande Rift in the
- east, and merges into the San Rafael Swell, another structural dome, to the
- north, and to the west it merges into the broad deformation of the Basin and
- Range Province.
- The Coldorado Plateau _is_ a sort of "window" of _reduced_
- deformation. It is very similar to the rest of the North American platform
- to the east, but it has been "cut off" by the Rio Grande Rift.
- There are processes that can uplift an area without causing a great
- deal of deformation. One is to heat up the underlying mantle. The Rio
- Grande Rift, and other relatively recent volcanism in the Coldorado Plateau
- area may be a partial indication of this process.
- Another factor that can produce the unconformities is sea-level
- variations. No, not "Biblical Flood"-style variations. I'm talking about
- sea-level variations on the order of 100m. There is good evidence, for
- instance, that the continental shelves were exposed, and therefore eroded,
- during the latest glaciations. Sea-level dropped because so much water was
- trapped in the ice caps. At the end of the last glaciation, the shelves
- were "flooded". There is some evidence for similar variations through most
- of the Earth's history, although the mechanism may not be glacial alone.
-
- Let's look at the effect of unconformities on the geologic history of an
- area, and how they complicate a flood model:
- One area I am familiar with is the South Mountain Batholith, in
- southern Nova Scotia. It is an agglomeration of dozens of smaller
- "granitic" bodies, and is approximately 100 X 40 km in surface dimensions.
- It extends to at least a kilometre depth, probably more. It occurs within
- metamorphosed sedimentary rocks of the Meguma Group, itself at least a
- kilometre or two thick, and composed of deep water marine sediments. The
- beds of the Meguma Group are extensively folded, in a similar fashion to a
- carpet pushed on its edge. The contact between the "granites" and the
- Meguma Group cuts across the tilted bedding, and it is easy to see places at
- the contact where the granite was injected into fractures, and where chunks
- of the Meguma Group were wedged off the wall of the magma chamber, sank into
- the melt, and were partly recrystallized. These chunks are called xenoliths
- or enclaves. Clearly the structures support the interpretation that the
- Meguma Group is older than the "granites", and since the "granites" are not
- folded as well, the folding of the Meguma Group must have occurred before
- the intrusion.
- On top of both the granites and the tilted beds of the Meguma Group
- are sediments of the Horton Group. The Horton Group contains plant fossils
- of Carboniferous age, but the fossils do not really matter. The basal
- contact of the Horton Group is erosive, and occurs with both the tilted beds
- of the Meguma Group (i.e. an angular unconformity) and the "granites" of the
- South Mountain Batholith. In the basal metre of the Horton Group, there are
- abundant pebbles of both the Meguma Group and the South Mountain Batholith.
- Often they are chemically altered, and rounded. Higher in the Horton Group,
- entire formations are composed of sandstones and conglomerates obviously
- derived from granitic sources (they contain much feldspar, quartz, and
- mica). Clearly the sequence of events in this area is:
- 1. deposit Meguma Group sediments in the ocean.
- 2. fold and metamorphose the sediments.
- 3. intrude the South Mountain Batholith (SMB).
- 4. solidify the SMB (it takes a _long_ time to cool).
- 5. erode the sediments on top, down to the level of the granites.
- 6. deposit Horton Group sediments on top of the erosion surface
- 7. fold and fault the Horton Group.
-
- And, there is yet another angular unconformity on top of the Horton
- Group, followed by more sediments (with fragments of the South Mountain
- Batholith, Meguma Group, and Horton Group), and basaltic lavas.
- Keep in mind that this is a great simplification of one corner of
- the North American continent. Geological history is very complex, even if
- you ignore fossils and radiometric dating entirely. Much more complex than
- flood models can easily explain.
-
- -Andrew
- macrae@pandora.geo.ucalgary.ca
-