"All continents (and large islands) are surrounded by a continental margin, a continuous band of mostly sedimentary rock.
This makes up some 20% of the ocean floor;
the rest is the deep ocean basins (abyssal plains).
The continental shelf is relatively flat, dipping down very gently (less than 0.1°) as it extends out from the shoreline to the shelf break or shelf edge, which is where the continental slope begins.
At the edge of the continental shelf, at a consistent average depth of about 430 ft., the slope of the seafloor suddenly increases from nearly flat to about 4°, all the way down to depths of 4,900 to 11,500 ft.. This is the continental slope, and if all the water were removed from the oceans, it would be the most conspicuous geomorphological boundary on Earth.
The sedimentary rocks within the continental margin can be extremely thick—over 12 miles deep in places, especially in buried basins.
Geomorphologist Lester King sum-marized:
Although few scientists address this issue, the continental shelf and slope are very difficult to explain within the uniformitarian (slow and gradual) paradigm.
Non-catastrophic processes would favor a gradual descent of sediments to the ocean depths. There really should be no continental shelf or slope.
King described the problem:
The reason there should be a gradual descent to the deep sea is that most ocean currents are wind-generated. (Sinking of denser, salty water at high latitudes is only a minor factor, although some scientists think otherwise.) Because of the prevailing winds, ocean currents are commonly parallel to the coast, such as the Gulf Stream off the East Coast of the United States. A uniformitarian would thus expect sediments to spread out first and then slide down into the deep ocean.
Sometimes, the dip of the sedimentary rocks in the continental margin increases seaward, forming what are called delta-like features. This indicates the depositional current was flowing offshore and not parallel to the shoreline as expected from wind-generated currents.
Hedberg states: “Reflection profiling has shown that many slopes in their present form are the result of prograding sedimentation.”
Prograding means that the sediment was deposited by currents that moved perpendicularly away from the continents, unlike the typical parallel-to-shore currents we see today.
Today, when a flooding river enters a larger body of water, it deposits its sediment load in the form of a delta.
---By analogy this sheds light on the origin of the continental shelf and slope.
*The top of the delta would represent the continental shelf;
*the delta edge would correspond to the continental slope.
--Continental margins represent a global phenomenon that gives powerful evidence for the global Flood.
This speaks strongly against the idea that the world’s sedimentary layers formed slowly over ‘millions of years’."
CMI
This makes up some 20% of the ocean floor;
the rest is the deep ocean basins (abyssal plains).
The continental shelf is relatively flat, dipping down very gently (less than 0.1°) as it extends out from the shoreline to the shelf break or shelf edge, which is where the continental slope begins.
At the edge of the continental shelf, at a consistent average depth of about 430 ft., the slope of the seafloor suddenly increases from nearly flat to about 4°, all the way down to depths of 4,900 to 11,500 ft.. This is the continental slope, and if all the water were removed from the oceans, it would be the most conspicuous geomorphological boundary on Earth.
The sedimentary rocks within the continental margin can be extremely thick—over 12 miles deep in places, especially in buried basins.
Geomorphologist Lester King sum-marized:
There have been repeated tectonic episodes: always in the same sense—the lands go up and the sea floor down…This is consistent with Psalm 104:8, describing the draining of the Flood water: “The mountains rose, the valleys sank down to the place that you appointed for them”.
Although few scientists address this issue, the continental shelf and slope are very difficult to explain within the uniformitarian (slow and gradual) paradigm.
Non-catastrophic processes would favor a gradual descent of sediments to the ocean depths. There really should be no continental shelf or slope.
King described the problem:
“Briefly the shelf is too wide, and towards the outer edge too deep, to have been controlled by normal wind-generated waves of the ocean surface”.Present processes would not form such a profile. Hedberg also stated, “…there is considerable controversy as to the origin in detail of continental slopes. It seems evident that there is no unique answer.”
The reason there should be a gradual descent to the deep sea is that most ocean currents are wind-generated. (Sinking of denser, salty water at high latitudes is only a minor factor, although some scientists think otherwise.) Because of the prevailing winds, ocean currents are commonly parallel to the coast, such as the Gulf Stream off the East Coast of the United States. A uniformitarian would thus expect sediments to spread out first and then slide down into the deep ocean.
Sometimes, the dip of the sedimentary rocks in the continental margin increases seaward, forming what are called delta-like features. This indicates the depositional current was flowing offshore and not parallel to the shoreline as expected from wind-generated currents.
Hedberg states: “Reflection profiling has shown that many slopes in their present form are the result of prograding sedimentation.”
Prograding means that the sediment was deposited by currents that moved perpendicularly away from the continents, unlike the typical parallel-to-shore currents we see today.
---By analogy this sheds light on the origin of the continental shelf and slope.
*The top of the delta would represent the continental shelf;
*the delta edge would correspond to the continental slope.
--Continental margins represent a global phenomenon that gives powerful evidence for the global Flood.
This speaks strongly against the idea that the world’s sedimentary layers formed slowly over ‘millions of years’."
CMI
