Andere Kunden interessierten sich auch für
![A Concise Geologic Time Scale]( "A Concise Geologic Time Scale")
A Concise Geologic Time Scale38,99 €![Science 101: Weather]( "Science 101: Weather")
Science 101: Weather17,99 €![The Essential Earth]( "The Essential Earth")
The Essential Earth338,99 €![Encyclopedia of Soil Science]( "Encyclopedia of Soil Science")
Encyclopedia of Soil Science330,99 €![Assessment of the Contribution of Small-scale Timber Production on Local Community's Livelihood in Mufindi District, Tanzania]( "Assessment of the Contribution of Small-scale Timber Production on Local Community's Livelihood in Mufindi District, Tanzania")
Assessment of the Contribution of Small-scale Timber Production on Local Community's Livelihood in Mufindi District, Tanzania47,95 €![Effective Rates Collection Via GIS Application. The Case of Lusaka City Council, Zambia]( "Effective Rates Collection Via GIS Application. The Case of Lusaka City Council, Zambia")
Effective Rates Collection Via GIS Application. The Case of Lusaka City Council, Zambia47,95 €![The Transgression of the Planetary Nitrogen Boundary. What is Germany's Internal and External Contribution?]( "The Transgression of the Planetary Nitrogen Boundary. What is Germany's Internal and External Contribution?")
The Transgression of the Planetary Nitrogen Boundary. What is Germany's Internal and External Contribution?17,95 €
Seminar paper from the year 2016 in the subject Earth Science / Geography - General, Basics, grade: 95%, Ruhr-University of Bochum (Institute of MIneralogy), course: Structural Geology, language: English, abstract: This assignment exhibits the period since Earth has formed until boundary conditions and tectonics started to stabilize. This period is called Precambrian and consists the 7/8 of Earth's history. Precambrian lasts 3,9 Ga and is separated into three Eons, Hadean, Archean and Proterozoic with respect to time occurrence.Earth loses heat through time due to gradually decrease in decay of radiogenic isotopes which are dispersed into the core, mantle and continental crust. Therefore, Earth composition and tectonics distinctly change. Tectonics generally change from vertical patterns to horizontal and the continental crust forms until the end of the Precambrian to the 82% of the overall crust, covering Earth now. Moreover, different movements of Supercontinents which fragmented, dispersed and collided where studied through geological, paleomagnetic and paleoclimatic studies.
Hinweis: Dieser Artikel kann nur an eine deutsche Lieferadresse ausgeliefert werden.
Hinweis: Dieser Artikel kann nur an eine deutsche Lieferadresse ausgeliefert werden.