module 1 Flashcards
what is our current understanding of the formation of the earth
-A dense cloud of gas and dust approx 4.5-4.6 million years ago and the dust collapsed
- this formed a solar nebula and at the center was hydrogen and helium which combined and released energy, and created the sun and 99% of avalible matter
- matter aggregated and formed things.
EVIDENCE: meterorites, meteroite craters, shooting stars, sample of solar system material
How do we get info about planetary age and composition
- isotopic dating
-radioactive isotopes decay (protons and neutrons leave randomly).
-they have a proportional decay rate and a half life - produces a unique parent and daughter isotope which can be used to determine planetary age
- tungson isopte used to date formation of earth and stars
what conditions are assumed for carbon dating
a)That the rock is not eroded or have lost material over time.
b)That the rock has not been contaminated while eroding
how and when did earth form?
-earth melts and minerals mixed
- iron and nickle begin to settle towards the center
- differentiated earth with light rock crust, intermediate density mantle, liquid outer core, nickle and iron core
how and when did the moon form
giant impact theory
- proto planet hits earth. ejection from this impact formed the moon
- created from proto planet and earth
how do other planets in the solar system differ from earth
terrestrial and non-terrestrial planets
terrestrial planets
- mercury, venus, earth and mars
- developed as hot rocky metals
-all have undergone differentiation - earth is THE ONLY ONE with tectonic plates which accounts for the structure of earth (mountains)
-theory that other terrestial planets has tectonic plates because of their structure (ie venus has mountains)
non terrestrial plantes
-formed from gases
- outer planets
- Jupiter Saturn, uranus, and neptune
scientific evidence of planet formation
- metereorites
-sample of solar system material
-shooting stars
meteroites
- may contain chondrules which are small particles solidified from molten droplets
- rich in iron and silion
-types:iron, stony-iron, chronrites, carbonaceous chondrites
periodic cycles in earth’s orbit
-changes in eccentrity
-axial precession
-changes in obliquity
earths layers
- crust
-upper mantle
-lower mantle
-outer core
-inner core