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Documents Geosc. 10: Unit 4 – The Blue Ridge The Blue Ridge Parkway, Virginia, in January, plus some other.....

Slide 1 Geosc. 10: Unit 4 – The Blue Ridge The Blue Ridge Parkway, Virginia, in January, plus some other Appalachian pictures. All photos by R. Alley The Blue Ridge runs…

Documents Mariner 10 Mercury Discovery Rupes (Discovery scarp) Thrust faults formed as the planet’s interior...

Slide 1 Mariner 10 Mercury Discovery Rupes (Discovery scarp) Thrust faults formed as the planet’s interior cooled and shrank, causing compression in the crust Slide 2 Tectonism…

Documents Plate Tectonics Or Do the continents move because they don’t like their neighbors?

Plate Tectonics Or Do the continents move because they donât like their neighbors? 19th century geologists wondered about the origin of mountains. How were they formed?…

Documents Types of plate boundaries

Types of plate boundaries Divergent plate boundary Oceanic spreading ridge Continental Rift zone New rock produced Convergent plate boundary Oceanic-oceanic convergence Continental-continental…

Documents MOUNTAIN AND MOUNTAIN RANGES A. Mountain

MOUNTAIN AND MOUNTAIN RANGES A. Mountain any part of the Earthâs surface sufficiently elevated above its surroundings to have a distinct summit and to be considered worthy…

Documents Evidence for Continental Movement Evidence for Continental Movement.

Evidence for Continental Movement Evidence of Continental Drift - The shape of coastlines match Philosopher Sir Francis Bacon remarked about this in 1620 Evidence of Continental…

Documents The Earth’s Evolving Crust. The Four Major Steps in the Formation of a Sedimentary Rock.

The Earthâs Evolving Crust The Four Major Steps in the Formation of a Sedimentary Rock 1. Weathering & Erosion 2. Transport 3. Deposition 4. Lithification Clastic Sediment:…

Documents Relative Dating

Relative Dating I. Relative Dating Relative Dating is when you give the age of a rock or fossil compared to another rock or fossil. Example: Rock A is OLDER than Rock B.…

Documents MOUNTAIN AND MOUNTAIN RANGES A. Mountain 1. any part of the Earth’s surface sufficiently elevated....

MOUNTAIN AND MOUNTAIN RANGES A. Mountain any part of the Earthâs surface sufficiently elevated above its surroundings to have a distinct summit and to be considered worthy…

Documents Chapter 12: Lithostratigraphy. Law of Superposition In any succession of strata, not disturbed or...

Chapter 12: Lithostratigraphy Law of Superposition In any succession of strata, not disturbed or overturned since deposited, younger rocks lie above older rocks. 1 2 3 4…