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The fossil record provides evidence for when organisms lived on Earth, how species evolved, and how some species have gone extinct. Geologists use a method called radiometric dating to determine the exact age of rocks and fossils in each layer of rock.
Those fossils that record the action of an organism, such as a footprint or burrow, are known as trace fossils. Paleontologists study fossils to help understand the evolution and the history of life on Earth. Fossils also tell us about ancient ecosystems and climates, and how climate change can affect life.
It is often found in deserts, beaches, and other sandy environments. Shale is formed from particles of mud. Good places to find fossils are outcrops. An outcrop is a place where old rock is exposed by wind and water erosion and by other people's digging.
Paleontological resources, or fossils, are any evidence of past life preserved in geologic context. They are a tangible connection to life, landscapes, and climates of the past. They show us how life, landscapes, and climate have changed over time and how living things responded to those changes.
Fossils give us a useful insight into the history of life on Earth. They can teach us where life and humans came from, show us how the Earth and our environment have changed through geological time, and how continents, now widely separated, were once connected.
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What Information Can Scientists Get From Fossils? Structure. The most basic information a fossil can provide is about what animals and plants looked like. ... Environment. The condition of a fossil can indicate what type of environment existed at the time. ... Dating. ... Geology. ... Evolution.
asphalt. a dark, sticky mixture; natural tar or pitch.

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