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How do we know what happened first?. James Hutton (1726-1797) Father of Modern Geology native of Edinburgh, Scotland educated as a medical doctor in Leiden.

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Presentation on theme: "How do we know what happened first?. James Hutton (1726-1797) Father of Modern Geology native of Edinburgh, Scotland educated as a medical doctor in Leiden."— Presentation transcript:

1 How do we know what happened first?

2 James Hutton ( ) Father of Modern Geology native of Edinburgh, Scotland educated as a medical doctor in Leiden (1749) passionate about scientific inquiry Historical Developments Theory of the Earth -- processes are slow; take a long time Charles Lyell ( ) Scotsman who attended Oxford University father was an avid naturalist rebelled against prevailing thought of catastrophism/Neptunism. Principles of Geology -- popularized Huttons views idea of uniformitarianism -- same processes operating today occurred in the past ….the present is the key to the past….

3 study of timing of geologic events and processes is geochronology Relative time order of events or objects from first (oldest) to last (youngest) she is older than he is; she was born first and he was born last age of events or objects expressed numerically she is twenty-one and he is nineteen Absolute time

4 Relative Time- this rock is older than that Principles Used to Determine Relative Age Unconformities Correlation The Standard Geologic Time Scale Index Fossils Absolute Time- this rock is 28 million years old Principles of radioactive decay

5 apply simple concepts to determine… original horizontality superposition lateral continuity cross-cutting relationships inclusions unconformities

6 original horizontality all beds originally deposited in water formed in horizontal layers sediments will settle to bottom and blanket the sea floor

7 Superposition: within a sequence of undisturbed sedimentary or volcanic rocks, layers become younger, upward

8 Lateral Continuity: original sedimentary layers extend laterally until it thins out at edges rocks that are otherwise similar, but are now separated by a valley or other erosional feature, can be assumed to be originally continuous. erosional

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10 cross-cutting relationships a disrupted pattern is older than the cause of the disruption e.g. an intrusion is younger than the rocks it intrudes

11 inclusions fragments of other rocks contained in a body of rock must be older than the host rock e.g. 1)xenoliths in granite are older than granite and 2) pieces of rock in conglomerate are older than conglomerate

12 unconformities A gap in the geologic record -- gap may be an amount of time or amount of missing section conformity relatively continuous deposition deposition of a sequence of parallel layers contacts between formations do not represent significant gaps in time

13 from: conformity

14 different types of unconformities 1. angular unconformity contact separates overlying younger layers from tilted older layers sequence of layers is not parallel contacts between formations may represent significant amounts of time angular unconformity

15 from: edu/envstudies/parks/rmgcan2.html

16 angular unconformity

17 different types of unconformities 2. disconformity contact separates beds (formations) that are parallel sequence of layers is parallel contacts between formations may represent significant amounts of time missing time is difficult to recognize

18 different types of unconformities 3. nonconformity strata deposited on older crystalline (metamorphic/igneous) rock erosion surface on igneous/metamorphic rock covered by sedimentary rocks large gap in geologic record nonconformity

19 Unconformity Types Using Grand Canyon as Example

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21 faunal succession (correlation by fossils) How is this done? index fossil short-lived organism; points to narrow range of geologic time fossil species succeed one another through the layers in a predictable order fossil assemblage group of fossils associated together

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