areas along hillsides.. & ..layers of sedimentary rock ..
Two kinds of fossils are body fossils, which preserve the actual remains or impressions of an ancient organism, and trace fossils, which are indirect evidence of an organism's activity, such as footprints or burrows.
There are a variety of types of fossils. These include cast fossils, mold fossils, petrified wood, as well as fossil fuels.
The best places to look for evidence of continental drift are paleontological evidence, such as similar fossils found on different continents that were once connected, and geological evidence, such as matching rock formations and mountain ranges on different continents. These can help support the theory of continental drift proposed by Alfred Wegener in the early 20th century.
If two widely separated layers of rock contain the same type of fossil, it suggests that the layers could be of similar age, as the presence of the same fossil indicates that the organisms lived during the same geological period. However, the environments of these layers may have been quite different, reflecting varying conditions such as climate, sedimentation, and water depth at the time of deposition. Fossils can be transported by various means, and thus, the same type of fossil in different environments might indicate migration or adaptability of the species. Therefore, while the fossils provide a chronological link, the differing environments suggest a complex history of ecological change.
Erosion
Two kinds of fossils are body fossils, which preserve the actual remains or impressions of an ancient organism, and trace fossils, which are indirect evidence of an organism's activity, such as footprints or burrows.
There are a variety of types of fossils. These include cast fossils, mold fossils, petrified wood, as well as fossil fuels.
The Benthic and Pelagic environments are the two main ocean environments.
to put them together like a puzzle or to look at the fossils that are found in 3 different continents
The two types of external organizational environments are the internal and the external organization environments.
well in your body there are made up of fossils as fossils are formed in hot places and your body is very warm
living and fossils
The Benthic and Pelagic environments are the two main ocean environments.
The best fossil evidence supporting the division between reptiles and birds would be transitional fossils showing a clear evolutionary pathway between the two groups. Fossils with features characteristic of both reptiles and birds, such as Archaeopteryx, provide strong support for the evolutionary link between these classes.
The best places to look for evidence of continental drift are paleontological evidence, such as similar fossils found on different continents that were once connected, and geological evidence, such as matching rock formations and mountain ranges on different continents. These can help support the theory of continental drift proposed by Alfred Wegener in the early 20th century.
Plants and animals
yes