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How would you correlate two rock units? On a field trip in the southwestern United States you would see some very unique rock layers. You might see a distinctive whitish rock unit that looks like sand dunes. This rock is the Navajo Sandstone. The first photo is from the Valley of Fire near Las Vegas, Nevada. The second is from Capitol Reef National Park in Utah. These sites are roughly 250 miles apart. Sand dunes stretched across this part of the country during the Mesozoic. When rock layers are in the same place, its easy to give them relative ages. But what if rock layers are far apart? What if they are on different continents? What evidence is used to match rock layers in different places? Widespread Rock Layers Some rock layers extend over a very wide area. They may be found on more than one continent or in more than one country. They are matched up by correlation. For example, the famous White Cliffs of Dover are on the coast of southeastern England. These distinctive rocks are matched by similar white cliffs in France, Belgium, Holland, Germany, and Denmark (Figure below). It is important that this chalk layer goes across the English Channel. The rock is so soft that the Channel Tunnel connecting England and France was carved into it! Chalk Cliffs. (A) Matching chalk cliffs in Denmark and (B) in Dover, U.K. Key Beds Like index fossils, key beds are used to match rock layers. A key bed is a thin layer of rock. The rock must be unique and widespread. For example, a key bed from around the time that the dinosaurs went extinct is very important. A thin layer of clay was deposited over much of Earths surface. The clay has large amount of the element iridium. Iridium is rare on Earth but common in asteroids. This unusual clay layer has been used to match rock up layers all over the world. It also led to the hypothesis that a giant asteroid struck Earth and caused the dinosaurs to go extinct. Using Index Fossils Index fossils are commonly used to match rock layers in different places (Figure below). If two rock layers have the same index fossils, then theyre probably about the same age. Using Index Fossils to match rock layers. Rock layers with the same index fossils must have formed at about the same time. The presence of more than one type of index fossil provides stronger evidence that rock layers are the same age. Summary A single rock unit contains the story of the geology of that location. To understand the geology of a region, scientists use correlation. To correlate rock units, something distinctive must be present in each. This can include an index fossil, a unique rock type, a key bed, or a unique sequence of rocks. A key bed can be global. An example is the iridium layer that was deposited at the time of the Cretaceous-Tertiary extinctions. Review What features must the iridium layer at the time of the dinosaur extinction need to be a key bed? To be more certain that fossils can be used to correlate rock layers, what is needed? What is the process of correlation? Use the resource below to answer the questions that follow. In what type of rock were the leaf fossils found? How is this type of rock formed? Why is this volcanic ash unique? How does the lapilli tuff form? What does the lapilli tuff allow scientists to do? LICENSED UNDER Relative age means the age of one object compared to the age of another object. Relative age does not tell the exact age of an object. The relative age of rocks and fossils can be determined using two basic methods: ordering of rock layers and index fossils: Ordering of Rock LayersScientists read the rock layers knowing that each layer is deposited on top of other layers.The law of superposition states that each rock layer is older than the one above it. So, the relative age of the rock or fossil in the rock or fossil in the rock is older if it is farther down in the rock layers.Relative dating can be used only when the rock layers have been preserved in their original sequence.Index FossilsCertain fossils, called index fossils, can be used to help find the relative age of rock layers. To be an index fossil -an organism must have lived only during a short part of Earths history;many fossils of the organisms must be found in rock layers;the fossil must be found over a wide area of Earth;the organism must be unique.The shorter time period a species lived, the better an index it is.Fossils that are found in many rock layers, therefore living long periods of time, do not qualify as index fossils. Click Here - to play the index fossil game! Complex layering due to intrusions and extrusions, faults, or unconformities can make dating rocks and fossils challenging. How do scientists accurately determine the age of rocks and fossils when each of these factors occur?Radioactive element decay can also be used to tell the age of fossils and rocks. How does this process work? Is it reliable? Why or why not?
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