State the principle of uniformitarianism. Explain how the law of superposition can be used to determine the relative age of rocks.
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1 Objectives State the principle of uniformitarianism. Explain how the law of superposition can be used to determine the relative age of rocks. Compare three types of unconformities. Apply the law of crosscutting relationships to determine the relative age of rocks.
2 # s 1 & 2 Uniformitarianism uniformitarianism a principle that geologic processes that occurred in the past can be explained by current geologic processes Geologists estimate that Earth is about 4.6 billion years old, an idea that was first proposed by James Hutton in the 18th century.
3 James Hutton
4 Uniformitarianism Hutton theorized that the same forces that change Earth s surface now, such as volcanism and erosion, are the same forces that were at work in the past. Hutton s ideas raised serious questions about Earth s age, because up until that time, most scientists thought Earth was only 6,000 years old, and that all Earth s geologic features had formed at the same time.
5 #3 Class discussion What reasoning did Hutton use to show that Earth is very old? Hutton reasoned that the extremely slow-working forces that changed the land on his farm has also slowly changed the rocks that make up Earth s crust.
6 # s 4 & 5 Relative Age, continued relative age the age of an object in relation to the ages of other objects One way to learn about Earth s past is to determine the order in which rock layers and other rock structures formed. Layers of rock, called strata, show the sequence of events that took place in the past.
7 Rock Strata: Look at the different layers
8 #6 Class discussion Why do geologists study strata? One way to learn about Earth s past is to determine the order in which rock layers and other rock structures formed.
9 # s 7 & 8 Relative Age, continued Scientists can determine the order in which rock layers formed by using a few basic principles. Once they know the order, a relative age can be determined for each layer. Relative age indicated that one layer is older or younger than another layer but does not indicate the rock s age in years.
10 #9 Law of Superposition, continued law of superposition the law that a sedimentary rock layer is older than the layers above it and younger than the layers below it if the layers are not disturbed
11 #10 Law of Superposition, continued Scientists commonly study the layers in sedimentary rocks to determine the relative age of rocks. Sedimentary rocks form when new sediments are deposited on top of old layers of sediment. As the sediments accumulate, they harden into layers called beds. The boundary between two beds is called a bedding plane.
12 Which layers are the oldest? Do you see how the rock layers on the left line up with the layers in the tower?
13 Law of Superposition, continued See page 187 for the law of superposition
14 #11 Class discussion Why does the law of superposition work is the rock layers are not disturbed? New sediments are deposited on top of old layers of sediment.
15 #12 Principle of Original Horizontality Scientist know that sedimentary rock generally forms in horizontal layers. The principle of original horizontality states that sedimentary rocks left undisturbed will remain in horizontal layers.
16 #13 Class discussion Why can scientists assume that sedimentary rock layers that are not horizontal have been tilted or deformed by crustal movements that happened after the layers formed? sedimentary rock generally forms in horizontal layers.
17 # s 14 & 15 Principle of Original Horizontality Graded Bedding In some cases, tectonic forces push older layers on top of younger ones or overturn a group of rock layers. So, scientists must look for clues to the original position of the layers. One clue is the size of particles in the layers. In some environments, the largest particles of sediment are deposited in the bottom layers.
18 #16 Principle of Original Horizontality Graded Bedding The arrangement of layers in which coarse and heavy particles are in the bottom layers is called graded bedding. If larger particles are located in the top layers, the layers may have been overturned by tectonic forces.
19 Principle of Original Horizontality, continued Graded Bedding
20 #17 Principle of Original Horizontality Cross-Beds Another clue is the shape of the bedding planes. When sand is deposited, sandy sediment forms curved beds at an angle to the bedding plane. These beds are called cross-beds. Scientists can study the shape of the cross-beds to determine the original position of the layers.
21 Principle of Original Horizontality, continued Cross-Beds
22 #18 Red Rock Canyon State Park Cross-Beds During most of its history, Red Rock Canyon was below a warm, shallow sea. Massive fault action and volcanic eruptions caused this seabed to begin rising some 225 million years ago.
23 # s 19 & 20 Red Rock Canyon State Park Cross-Beds As the waters receded, sea creatures died, and the calcium in their bodies combined with sea minerals to form limestone cliffs studded with ancient fossils. Some 45 million years later, the region was buried beneath thousands of feet of windblown sand. As time progressed, iron oxide and calcium carbonate infiltrated the sand, consolidating it into cross-bedded rock.
24 Red Rock Canyon State Park
25 Red Rock Canyon State Park
26 Red Rock Canyon State Park
27 Red Rock Canyon State Park
28 #21 Class discussion What layer should be on top in Red Rock Canyon Park? sandstone
29 #22 Principle of Original Horizontality Ripple Marks Ripple marks are small waves that form on the surface of sand because of the action of water or wind. When the sand becomes sandstone, the ripple marks may be preserved. In undisturbed sedimentary rock layers, the crests of the ripple marks point upward. Scientists study the orientation of the ripple marks to determine the original position of the layers.
30 Principle of Original Horizontality, continued Ripple Marks
31 Principle of Original Horizontality, continued Ripple Marks
32 #23 Class discussion How can ripple marks indicate the original position of rock layers? Because ripple marks form at the top of a rock layer, scientists can use the orientation of the ripple marks to determine which direction was up when the rock layers formed.
33 #24 Unconformities, continued unconformity a break in the geologic record created when rock layers are eroded or when sediment is not deposited for a long period of time Movements of Earth s crust can lift up rock layers that were buried and expose them to erosion. Then, if sediments are deposited, new rock layers form in place of the eroded layers. The missing layers create a break in the geologic record, called an unconformity.
34 #25 Unconformities, continued There are three types of unconformities. A nonconformity is an unconformity in which stratified rock rests upon unstratified rock. An angular unconformity is the boundary between a set of tilted layers and a set of horizontal layers. A disconformity is the boundary between horizontal layers of old rock and younger, overlying layers that are deposited on an eroded surface.
35 Types of Unconformities, continued See page 189 for the types of unconformities
36 Nonconformity
37 Angular unconformity
38 Disconformity
39 #26 Unconformities, continued Crosscutting Relationships law of crosscutting relationships the principle that a fault or body of rock is younger than any other body of rock that it cuts through.
40 #27 Unconformities, continued A fault is a break or crack in Earth s crust along which rocks shift their position. An intrusion is a mass of igneous rock that forms when magma is injected into rock. In these cases, scientists use the law of crosscutting relationships, or the fact that a fault or an intrusion is always younger than the layers it cuts through, to determine the order of the layers.
41 Unconformities, continued Cross-cutting Relationships of Surface Features on Europa
42 Unconformities, continued A fault
43 #28 Crosscutting Relationships, continued See page 190 for crosscutting relationships
44 List events or layers in order. Superposition Picture Earthquake (Fault line) Deposit D Deposit B Deposit G Intrusive Lava Deposit R River cuts through Deposit E Deposit
45 List events or layers in order. Superposition Picture 3 rd Earthquake (Fault line) 9 th Deposit D 5 th Deposit B 2 nd Deposit G 4 th? Intrusive Lava 1 st Deposit R 6 th River cuts through 7 th Deposit E 8 th Deposit A
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