In disturbed sediments without layers, the relative age of the sediments would be unknown.
Normally, the oldest rocks are found at the bottom of the layers, being the first of the sediments that were deposited.
FALSE
Sedimentation of transported weathered and eroded material is continuous, cyclical, or event based. New sediments are deposited on top of existing sediments, forming layers that may be visible in a sedimentary rock body.
The chronological order of rock layers is usually determined by their order in an undisturbed sequence of strata. According to the principle of superposition, the oldest layers would be found at the bottom and the youngest layers at the top. In disturbed rock layers (those that have been folded, uplifted, or generally disrupted by tectonic forces), the determination must be made based on the presence of index fossils, comparison to undisturbed strata or radiometric dating.
It would be found in the lower layers, rather that younger fossils which are found in the upper layers. ♥
Normally, the oldest rocks are found at the bottom of the layers, being the first of the sediments that were deposited.
true A+
true A+
FALSE
because they are sedimentary rock
Deep in the ground.
The furthest down of all top layers.
the theory that layer of sediments are geologically younger than the layers found below it
Sedimentation of transported weathered and eroded material is continuous, cyclical, or event based. New sediments are deposited on top of existing sediments, forming layers that may be visible in a sedimentary rock body.
in the lowest layers of rock
in the lowest layers of rock
The chronological order of rock layers is usually determined by their order in an undisturbed sequence of strata. According to the principle of superposition, the oldest layers would be found at the bottom and the youngest layers at the top. In disturbed rock layers (those that have been folded, uplifted, or generally disrupted by tectonic forces), the determination must be made based on the presence of index fossils, comparison to undisturbed strata or radiometric dating.