Geological time Flashcards
(16 cards)
What does deep time tell us?
Discovery of the antiquity of the Earth is the most important discovery that the science of geology has made (Earth = ~4.6 billion years)
Define archbishop Ussher:
analyzed biblical scriptures and studied genealogies to calculate the age of the Earth (~6 thousand years)
Define relative geological ages:
great for sedimentary rock; based upon order of formation. Determination of older vs. younger relationships.
9 Principles of geology:
- Principle of uniformism
- superposition
- lateral continuity
- cross-cutting relationship
- baked contacts
- inclusions
- fossil succession
- unconformities
Principle of uniformism:
developed by James Hutton in the Scottish highlands. The present is the key to the past!!
Superposition:
In an undisturbed succession of sedimentary rock layers, the oldest layer is at the bottom and the youngest layer is at the top.
Original horizontal:
Sediments settle out by gravity. This causes sediments to accumulate horizontally. So, tilted sedimentary rocks must be deformed.
Lateral continuity:
Sedimentary layers usually accumulate in continuous sheets in a given region. They will be continuous either until they pinch out at their margins or are cut (by a river, stream, etc.)
Cross-cutting relations:
Younger features truncate (cut across) older features. Faults, dikes, erosion, etc., must be younger than the material that is faulted, intruded, or eroded.
Baked contacts:
An igneous intrusion will bake or metamorphose the surrounding rocks.
Inclusions:
Where a rock fragment is found within another. Inclusions are always older than the rock they are in.
Fossil Succession:
Fossils are often preserved in sedimentary rocks. Fossils indicate past depositional environments and correlate strata. Specific fossils are only found within a limited time range (Index Fossils).
Unconformities:
represents a gap in time from non-deposition or erosion
Angular unconformity:
Rocks below this unconformity were tilted or folded before the unconformity developed
Nonconformity:
igneous/metamorphic rocks overlain by sedimentary rocks.
Disconformities:
occur between parallel layers of sedimentary rocks.