The three kinds of information can geologists gather from a study of fossils is amber fossil, trace fossil, and the carbon film. Wait a second, no that's not right. Those are just three kinds of fossils. Those aren't three kinds of information.
1. Fossils tell scientists the types and sizes of animals that lived in the distant past;
2. Tests made on fossils tell scientists approximately how long ago they lived;
3. The types of materials in which fossils are found tell scientists the area where the fossil first died, the cooling rates of some different materials, and the times of lava flows, as well as other items of information;
4. Comparing different fossils of the same type, from different areas, tells scientists the times of certain geologic events, such as an ice age, or a volcanic eruption;5. The layers of rock (or soil) in which fossils are found can tell scientists some of the geologic history of the geographical area in which the fossil was found. For example, sometimes seashell fossils are found in the rock of high mountains! That can only mean that the high mountain was once on the floor of an ocean or river. Over time, plate movement, volcanic eruption, and earthquakes have moved the old ocean floor (or river bottom) 'way up to the top of a mountain
There you go.
Relative age of the rocks and the Paleo environment.
the answer is elemetary
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.
Petrified fossils: where organic material is replaced by minerals. Mold fossils: where the shape of an organism is preserved in sediment. Cast fossils: formed when a mold fills with minerals, creating a replica of the organism. Trace fossils: records of biological activity, like footprints or burrows. Amber fossils: organisms preserved in hardened tree resin.
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).
The three kinds of information can geologists gather from a study of fossils is amber fossil, trace fossil, and the carbon film. Wait a second, no that's not right. Those are just three kinds of fossils. Those aren't three kinds of information.1. Fossils tell scientists the types and sizes of animals that lived in the distant past;2. Tests made on fossils tell scientists approximately how long ago they lived;3. The types of materials in which fossils are found tell scientists the area where the fossil first died, the cooling rates of some different materials, and the times of lava flows, as well as other items of information;4. Comparing different fossils of the same type, from different areas, tells scientists the times of certain geologic events, such as an ice age, or a volcanic eruption;5. The layers of rock (or soil) in which fossils are found can tell scientists some of the geologic history of the geographical area in which the fossil was found. For example, sometimes seashell fossils are found in the rock of high mountains! That can only mean that the high mountain was once on the floor of an ocean or river. Over time, plate movement, volcanic eruption, and earthquakes have moved the old ocean floor (or river bottom) 'way up to the top of a mountainThere you go.
The three kinds of information can geologists gather from a study of fossils is amber fossil, trace fossil, and the carbon film. Wait a second, no that's not right. Those are just three kinds of fossils. Those aren't three kinds of information.1. Fossils tell scientists the types and sizes of animals that lived in the distant past;2. Tests made on fossils tell scientists approximately how long ago they lived;3. The types of materials in which fossils are found tell scientists the area where the fossil first died, the cooling rates of some different materials, and the times of lava flows, as well as other items of information;4. Comparing different fossils of the same type, from different areas, tells scientists the times of certain geologic events, such as an ice age, or a volcanic eruption;5. The layers of rock (or soil) in which fossils are found can tell scientists some of the geologic history of the geographical area in which the fossil was found. For example, sometimes seashell fossils are found in the rock of high mountains! That can only mean that the high mountain was once on the floor of an ocean or river. Over time, plate movement, volcanic eruption, and earthquakes have moved the old ocean floor (or river bottom) 'way up to the top of a mountainThere you go.
information specifc to the fourm
The three kinds of information can geologists gather from a study of fossils is amber fossil, trace fossil, and the carbon film. Wait a second, no that's not right. Those are just three kinds of fossils. Those aren't three kinds of information.1. Fossils tell scientists the types and sizes of animals that lived in the distant past;2. Tests made on fossils tell scientists approximately how long ago they lived;3. The types of materials in which fossils are found tell scientists the area where the fossil first died, the cooling rates of some different materials, and the times of lava flows, as well as other items of information;4. Comparing different fossils of the same type, from different areas, tells scientists the times of certain geologic events, such as an ice age, or a volcanic eruption;5. The layers of rock (or soil) in which fossils are found can tell scientists some of the geologic history of the geographical area in which the fossil was found. For example, sometimes seashell fossils are found in the rock of high mountains! That can only mean that the high mountain was once on the floor of an ocean or river. Over time, plate movement, volcanic eruption, and earthquakes have moved the old ocean floor (or river bottom) 'way up to the top of a mountainThere you go.
Relative age of the rocks and the Paleo environment.
The six types of fossils are called:body fossilstrace fossilsmolecular fossilsressin fossilsmicrofossilspseudofossilsliving fossils
the answer is elemetary
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.
living and fossils
Scientists gather information that earth is continually changing by observing tectonic plate movements and studying how the layers of the crust were formed. For example, the continental drift is the idea of the continents that were all together the the years passed and the continents got separate. This idea was first suggested by Alfred Wegener in 1915. He called the single large continent Pangea. Today, there are many kinds of evidence that support continental movement. The evidence include: In 1858: Geologist Eduard Seuss points out that fossils of the Glossopteris plant were found in 5 continents and in India. Also, In 1965: Geologist Edward Bullard uses computers to match coats of South America and Africa. They match extremely well at an ocean depth of 1,000 m.
maybe a Sonar
e each fossils