Continental Drift Alfred Wegener 1915 Continental Jigsaw Puzzle

  • Slides: 27
Download presentation
Continental Drift • Alfred Wegener – 1915 • Continental Jigsaw Puzzle – Fossils Matched

Continental Drift • Alfred Wegener – 1915 • Continental Jigsaw Puzzle – Fossils Matched across the sea – Common rock types (Africa and Appalachian) – Ancient Climates

Fossil and Rock Evidence

Fossil and Rock Evidence

Rejected • There was no credible mechanism for the movement of continents

Rejected • There was no credible mechanism for the movement of continents

Theory of Plate Tectonics • WWII oceanographers – large picture of the ocean floor.

Theory of Plate Tectonics • WWII oceanographers – large picture of the ocean floor. Ocean ridges • Ocean drilling – established the age of the ocean floor • Paleomagnetism

Age of Ocean Floor

Age of Ocean Floor

paleomagnetism

paleomagnetism

Plate boundaries

Plate boundaries

Divergent boundaries

Divergent boundaries

Rift zone

Rift zone

Convergent boundaries •

Convergent boundaries •

Volcanic formation

Volcanic formation

Transform boundary

Transform boundary

How is sediment formed • Weathering • Mass wasting • Erosion

How is sediment formed • Weathering • Mass wasting • Erosion

Weathering • Rocks are broken down to sediment through the process of either –

Weathering • Rocks are broken down to sediment through the process of either – Mechanical weathering – Chemical weathering

Mechanical Weathering – Physical breaking up of rock - disintegration – Rock is broken

Mechanical Weathering – Physical breaking up of rock - disintegration – Rock is broken into smaller pieces • Frost Wedging • Sheeting • Biological activity

Frost Wedging

Frost Wedging

Sheeting

Sheeting

Biological weathering

Biological weathering

Chemical Weathering • Alters internal structure of the mineral by removing and/or adding elements

Chemical Weathering • Alters internal structure of the mineral by removing and/or adding elements – Oxidation – Carbonic Acid

Oxidation • Water is the agent of chemical weathering. • Oxygen dissolved in water

Oxidation • Water is the agent of chemical weathering. • Oxygen dissolved in water will oxidize iron-rich minerals

Carbonic acid • Carbon dioxide dissolved in water forms a weak acid. This weak

Carbonic acid • Carbon dioxide dissolved in water forms a weak acid. This weak acid will react with mineral elements; breaking the rock down.

Mass Wasting • The transfer of rock and soil downslope, under the influence of

Mass Wasting • The transfer of rock and soil downslope, under the influence of gravity. – Mudslide – Rockslide – Earthflow – slump

Triggers of Mass Wasting Over saturation of land Over steepened slopes Loss of vegetation

Triggers of Mass Wasting Over saturation of land Over steepened slopes Loss of vegetation Earthquakes

Erosion • The physical removal of material by a mobile agent such as flowing

Erosion • The physical removal of material by a mobile agent such as flowing water, waves, wind or ice • Water • Wind

Soil • Combination of sediment and organic matter

Soil • Combination of sediment and organic matter