older fossils are usually further in the earth because the creature died before the others so the go down further and the ones that dies more recently are closer because they died more recently so haven't had the time to move further before they where found
The basement is a term sometimes used, and Cratonis another used in a continental context.The Principle of Superposition has it that in a given formation, the top layers are the youngest, and the deeper layers the oldest.
Undistributed rock layers may indicate that the layers have not been disturbed or deformed from their original horizontal positions. The oldest rock layers are typically found at the bottom of a sequence, while the youngest rock layers are found at the top, following the principle of superposition in geology.
The oldest organisms can generally be found in the lower layers of rock, as these layers were formed earlier than the upper layers. By examining the relative positions of different rock layers, scientists can determine the ages of the organisms found within them.
on th ebottom
In undisturbed rock layers, the principle of superposition states that the youngest rock layers are on top and the oldest are at the bottom. This means that the rock layer closest to the surface is the youngest, while the layer at the bottom is the oldest. Additionally, the principle of cross-cutting relationships helps determine relative ages by looking at how faults and intrusions cut across rock layers.
Sandstone is a sedimentary rock. Sedimentary rocks form from sediments that deposited by the wind and water. Over the time those sediments will get pressed and cemented together. It can take millions of years for sediments to become a rock. So the oldest layers of a sandstone are on a bottom.
The basement is a term sometimes used, and Cratonis another used in a continental context.The Principle of Superposition has it that in a given formation, the top layers are the youngest, and the deeper layers the oldest.
The oldest fossils are typically found in the deepest sedimentary rock layers, which are located at the bottom of a rock formation. This principle is known as the law of superposition in geology, where older rock layers are found beneath younger ones.
The geologic law that scientists use to date the crust by studying the layers of rocks is the Law of Superposition. This law states that in a sequence of undisturbed rock layers, the oldest rock layer will be at the bottom and the youngest will be at the top. By studying the relative positions of these rock layers, scientists can determine the relative ages of the rocks.
Undistributed rock layers may indicate that the layers have not been disturbed or deformed from their original horizontal positions. The oldest rock layers are typically found at the bottom of a sequence, while the youngest rock layers are found at the top, following the principle of superposition in geology.
The simple answer is that the old rock is at the bottom and the young rock is at the top. But sometimes the Earth has folded its skin over so it's all sideways or even upside down. You can see seashells at 5,000 metres up the Himalayas. The newest rocks are those formed where the crust is spreading, or as lava flows from volcanoes. This rock was liquified and mixed in its magma form. The oldest rocks are near the centers of continents, mainly underground but occasionally exposed by upthrust folding and/or erosion.
The oldest rocks (layers) are at the bottom. The youngestrocks (layers) are at the top
The undisturbed rock layers are horizontal and in order of age from youngest nearest the surface to oldest at the bottom of the rock unit.
The oldest organisms can generally be found in the lower layers of rock, as these layers were formed earlier than the upper layers. By examining the relative positions of different rock layers, scientists can determine the ages of the organisms found within them.
The oldest layers of sediments are typically found at the bottom of a sedimentary rock sequence, with the youngest layers at the top. Over time, new layers of sediments accumulate on top of older layers, creating a chronological sequence with the oldest layers at the bottom.
Deep in the ground.
on th ebottom