Astron notes - Google Docs PDF

Title Astron notes - Google Docs
Course Introduction to Astronomy and Astrophysics
Institution McMaster University
Pages 11
File Size 165.2 KB
File Type PDF
Total Downloads 49
Total Views 148

Summary

Here are the notes I took for chapter 11-13 they are pretty fire....


Description

Chapter 10: Venus and Mars. ➔ ➔ Venus ◆ .72 AU ◆ P = 225 ➔ Mars ◆ 1.52 AU ◆ P = 687 ➔ Because venus is in earth orbit we can see it either in evening in west after sunset or morning in the east before sunrise ➔ Because mars is outside we can see it anywhere on the ecliptic. ➔ Venus similar density to earth (5.2 g/cm) ◆ Similar radius ◆ temperature is alot higher ◆ pressure is alot higher ➔ Mars half earth size and lower density (3.9g/cm) ◆ colder than earth ◆ Thin atmosphere ➔ From earth venus is bright because it is close and also very reflected ◆ 17% of sunlight reflected ◆ This is because venus is covered in clouds ● Cant see surface with optical telescope ➔ From earth mars has a redish tinge due to iron oxides (rust) ◆ Regolith - soil on surface of mars ◆ We can see features and color variations/icecaps on mars ➔ Mars tilted at 25 degrees ◆ This allows it to have seasons similar to earth ◆ Day is 24 hours 37.5 mins ➔ Venus has a retrograde spin ◆ Cloud layre stoped us from determining rotation period until 1960s ● Radar was then bounced on planet to determined spin period ◆ Rotation period is 243 days (siderial day) ◆ Retrograde means looking above from the north pole it spins clockwise (earth spins counterclockwise) ◆ Venus year only 225 days ● Sun rises in west on venus when you put those motions together. ◆ Venus solar day only 117 days ◆ Retrograde spin theorized to be cause by large collision early in solar system ➔ Record time lander alive on venus 127 mins before it melted ➔ No erosion on venus ◆ Too hot for water or ice to exist so they cannot cause erosion ◆ Wind speed too low to cause erosion ➔ Volcanoes, impact craters and other features in crust ◆ No evidence for plat tectonics















➔ ➔

◆ Convection occurs in mantled ● Evidenced by stress features ○ Folds faults ridges and cracks ● No movement so no subduction zones. Much of surface consists of low lying lava planes like lunar mare ◆ Highlands: aphrodite and ishtar ● Both result of crust compression ● Maintained by mantle convection Many volcanoes ◆ Some evidence that they are active ◆ Some similar to our volcanoes ◆ Some have pancake dome-like structures Impactors ◆ 30km useful for dating Surface age: 300-600 million years (young!) ◆ Seems to have undergone planet wide resurfacing from some kind of volcanic convulsion Venus atmosphere ◆ Hot, dry, calm winds ◆ 96.5% CO2 ◆ 3.5% N2 ◆ 150ppm SO2 ◆ 20ppm H2O ◆ Pressure: 90 bars (equal to under 1km of water on earth) ◆ Sulphuric acid rain from clouds at top of atmosphere ◆ Troposphere at least 50km Phosphene found on venus ◆ Only know to be produced by life ◆ Could mean life on venus ◆ No explanation right now Surface temp ◆ 700+ kelvin ◆ due to runaway greenhouse effect ◆ Could have had oceans that evaporated due to sun releasing more energy Mars cold and dry ◆ May have once had water No sample return from mars ◆ We have samples from martian meteorites ◆ Rock ejected with lower escape velocity on mars due to less mass ◆ Samples contain gas bubbles, water, carbonbased compounds.

◆ Rocks have water and carbon based compounds in them suggesting presence of water and possibly life ➔ Mars overview ◆ Mostly silicate (low dense), small metal core ◆ Core thought to be solid because planet is smaller and we think it has had time to cool quicker than earth ◆ Supported by lack of global magnet field on mars ◆ Mars has local strong magnetic fields suggesting there was a strong magnetic field in the past ◆ Mars about half heavily cratered highland terrain mostly found in southern hemisphere ◆ Other half younger low lying volcanic plains in north ◆ Mars has lot of volcanoes ● Tharsis bulge is volcainic region ● On top is highest peak in solar system ○ Olympus mons: 20km high (3x taller than tallest earth mountain) ● Upswelling of tharsis bulge caused techtonic cracking of crust ○ Vallis marineris: massiv valley formed from cracking (not canyon because not cut by water) ○ Has experienced water erosion(earlier) and wind (still today) ◆ Surface ● Made of clay and iron oxides (reddish color) ● 35c to -143c ● Ice for h2o and co2 (dry ice) ● Atmosphere very thin ○...


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