A layer of rock containing fossils at high elevations, such as in a mountain wall, indicates that those sediments were once deposited in a marine environment, like a shallow sea, which has since been uplifted due to tectonic forces. Over millions of years, geological processes such as plate tectonics, erosion, and sedimentation can elevate these fossil-rich layers to their current position. This phenomenon underscores the dynamic nature of Earth's geology, where ancient seafloor sediments can become part of towering mountain ranges through processes like folding and faulting.
The sediments which make up the rocks on the highest mountains were once at the bottom of an ocean, (where the animals lived), and were only pushed up by the action of Plate Tectonics.
The discovery of fossils on mountain tops supports the theory of plate tectonics, as it indicates that these areas were once at lower elevations where fossils could form. Over time, the movement of tectonic plates pushed these areas upwards to form mountains, carrying the fossils with them. This provides evidence of the dynamic nature of the Earth's crust and the processes that shape the planet's surface.
Fosssils are the preserved remains or traces of animals , plants, and other organisms from the remote past. The totality of fossils, both discovered and undiscovered, and their placement in fossiliferous (fossil-containing) rock formations and sedimentary layers (strata) is known as the fossil record.Types:-mold fossils (a fossilized impression made in the substrate - a negative image of the organism)cast fossils (formed when a mold is filled in)trace fossils = ichnofossils (fossilized nests, gastroliths, burrows, footprints, etc.)true form fossils (fossils of the actual animal or animal part).
Fossils found in rock at the top of mountains indicate that the rock was once at the bottom of a body of water because the fossils are typically of marine organisms that lived in water. The presence of marine fossils in mountain rock suggests that the rock was uplifted from below sea level to its current position at the mountain top over millions of years.
The occurrence of marine fossils in rock strata located high in terrestrial mountain ranges can be attributed to the process of tectonic plate movement. These fossils were originally deposited in seabeds and later uplifted as the plates collided and formed mountain ranges through processes like orogeny. This uplift may have occurred over millions of years, resulting in the marine fossils being exposed at high elevations today.
The sediments which make up the rocks on the highest mountains were once at the bottom of an ocean, (where the animals lived), and were only pushed up by the action of Plate Tectonics.
550 million years old
Containing fossils with traces of plant or animal life.
its part of the rock cycle
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Fossil rocks are rocks containing the bones of ancient animals like dinosaurs. Also the shells of clams, snails, sea urchins, corals, plants: in fact the remains, traces or indications of life in the past
If the rocks containing the fossils have been involved in a mountain building episode they would be folded and if some of the folds were laid in a recumbent position and later eroded you would have older above younger rocks. Of course, it would be easy to find out if this was the case because of the various sedimentary structures in each separate layer of rock.
yes
The discovery of fossils on mountain tops supports the theory of plate tectonics, as it indicates that these areas were once at lower elevations where fossils could form. Over time, the movement of tectonic plates pushed these areas upwards to form mountains, carrying the fossils with them. This provides evidence of the dynamic nature of the Earth's crust and the processes that shape the planet's surface.
put in frezzer
Fossils, rock layers, and mountain ranges were some of the land features that provided evidence for Wegener's hypothesis of continental drift.
The Adirondack rocks have been both severely folded and sheared by ductile deformation and shattered by brittle.