Lecture 2 Flashcards
Earth’s Internal Structure
Inner Core- extremely hot and solid. Asthenosphere (upper mantle) is composed of solid, hot magma with some flow. Lithosphere is a thin and brittle crust.
Mechanisms of Plate boundries
Divergent, Convergent, Transform and Plate boundary zone.
what is the motor
the mantle . Plate movement is driven by mantle convection
Describe the rock cycle
Metamorphic- metamorphism- melting and metamorphism and internal heat causes igneous rocks- weathering and erosion creates sediments- deposition and lithification creates sedimentary rocks. metamorphism creates metamorphic`
The alkali feldspar
is Any of the group of feldspars rich in sodium and/or potassium. low is silica and temperature and water rich.
Hyrdrologic cycle
Movement of water from oceans to atmosphere and back. solar energy drives movement of water.
Biogeochemical cycle
Combines the three previous cycles. transfer of chemical elements through a series of reservoirs. many important chem.ical elements are not well understood. (C,N,P)
EarthQuakes how many events 1963-1998
358,214 events
types of volcanoe
subduction zones, mid-ocean ridges and hot spots (flood basalts)
Jet stream
A narrow, variable band of very strong, predominantly westerly air currents encircling the globe several miles above the earth.
fundamental concepts for understanding natural processess
- Hazards are predictable from scientific evaluation.2 risk analysis is an important component in our understanding of the effects of hazardous processes. Linkages exist between different natural hazards as well as between hazards and the physical environment. Hazardous events that previously produced disasters are now producing catastrophes. consequences of hazards can be minimized.