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The Scale of the Cosmos
The Scale of the Cosmos

... • Accelerating a spaceship close to the speed of light takes huge amounts of energy. • Even if you travel more slowly, your rocket would require massive amounts of fuel. • If you were piloting a spaceship with the mass of 100 tons (the size of a yacht) to the nearest star 4 ly away, and you wanted t ...
Lecture 1: Nucleosynthesis, solar composition, chondrites, volatility
Lecture 1: Nucleosynthesis, solar composition, chondrites, volatility

... bulk solar system composition and hence may be close to bulk earth composition ...
Name: Date:
Name: Date:

... 2. How are the inner planets different from the outer planets? ___________________________ _____________________________________________________________________ ...
The Earth - for physicists - University of California, Riverside
The Earth - for physicists - University of California, Riverside

... The Earth’s history is divided into four eons: Hadean, Archean, Proterozoic and Phanerozoic. When I was a child, the “Cambrian era” was as far back as my textbooks went, except for the murky “Precambrian”. But the Cambrian began just 540 million years ago. The Cambrian marks the start of the current ...
Venus - University of Chicago Math
Venus - University of Chicago Math

... the same as the pressure at a depth of 1 km in Earth’s oceans) • mostly CO2 • Several layers of clouds many km thick composed of sulfuric acid (the acid in acid rain) • runaway greenhouse effect (temperature at the surface is hot enough to melt lead) ...
DOC
DOC

... the seasons ...
From Here on Earth
From Here on Earth

... Coronae are one of the few quantum colour effects that can be easily seen with the naked eye. This type of solar corona is due to water in the Earth's atmosphere and is altogether different from the solar corona that exists continually around the Sun so it stands out during a total solar eclipse. Th ...
Astronomy Teleclass Webinar!
Astronomy Teleclass Webinar!

... The Sun rotates once every 27 days at its equator and 31 days at the poles.  The core temperature of the Sun is 15 million degrees Celsius.  A planet has three criteria: It orbits the Sun, has cleared its orbit of smaller objects, and is large  enough so its own gravity makes it round.  There are th ...
Chapter 29 Our Solar System
Chapter 29 Our Solar System

... 1. A cloud of ____________________ that stars & planets are formed from 2. Consists mainly of _________________ & _________________gas 3. Condenses due to ________________ & concentrates to form stars or planets 4. As it condenses, the cloud _____________, becomes __________ like a disk, and _______ ...
Origin of the atmosphere and ocean First read this verse: Earth`s
Origin of the atmosphere and ocean First read this verse: Earth`s

... beginning of the Geologic History on Earth. At this stage, the Earth lost its original gas envelope and its crust became cool. • The volcanic activity and meteor bombardment were still intense until 3.9 billion yrs. ...
File
File

... ranges from 801 ° F on the side facing the sun to -279 ° F on the side facing away from the sun. The lack of atmosphere on Mercury means that we can see its surface directly, which is gray in color and is covered with craters. Venus is the second planet away from the sun and is named after the Roman ...
THE SOLAR SYSTEM
THE SOLAR SYSTEM

... Jovian). Pluto is considered by many astronomers to no longer be a planet, since there are now several known objects in orbits similar to Pluto's and of similar size - these are believed to be members of the Kuiper-belt. In addition to the major planets, there are a large number of moons, asteroids, ...
Intro to Astronomy
Intro to Astronomy

... • Although the Earth’s distance from the Sun changes slightly as it orbits, the distance is not great enough to cause a substantial change in the climate. • The tilt of the Earth (23.5o) is what causes the seasons to change. • During the summer, the Northern Hemisphere is titled towards the Sun, whi ...
The Moon and the Sun: 2003 version
The Moon and the Sun: 2003 version

...  When it is getting smaller, the Moon is waning.  When the Moon is more than half-lit, it is called a gibbous Moon.  When the moon is less than half-lit, it is called a crescent Moon. ...
Earth in Space - 7-8WMS
Earth in Space - 7-8WMS

... During the time (from “new moon” to “full moon”, the Moon is said to be waxing (showing more brightness). During the next two weeks (after “full moon”), the Moon gradually changes from all light (the “full moon”) back to all dark (the “new moon”). During this time the Moon is said to be waning (sho ...
Subject: Earth Science Grade: 11 Unit #: 1 Title: Astronomy
Subject: Earth Science Grade: 11 Unit #: 1 Title: Astronomy

... galaxy and the galaxy’s place in the universe. The students will have to incorporate the Sun’s influence on the Earth. They will show understanding of how Earth’s orbit, the Moon’s orbit, and gravitation are related to the Sun and each other. They will need to discuss what comets and asteroids are a ...
Origin of Modern Astronomy
Origin of Modern Astronomy

... 1. The path of each planet around the sun is an ellipse, with the sun at one focus. The other focus is symmetrically located at the opposite end of the ellipse. 2. Each planet revolves so that an imaginary line connecting it to the sun sweeps over equal areas in equal time intervals. If a planet is ...
Science 1 (MillinerSci1)
Science 1 (MillinerSci1)

... 12. Which tool is used by astronomers to make objects that are far away appear larger? A. microscope B. satellite C. spacecraft D. telescope 13. In a family of rabbits, half the rabbits are brown and half are white. Which statement BEST explains why the rabbits have two different colors? A. The whit ...
Sun, Moon and Stars - Siemens Science Day
Sun, Moon and Stars - Siemens Science Day

... Milky Way – A system that can be comprised of millions of stars that have their own solar systems Solar System – (Our solar system) includes the sun with its planets and their natural satellites such as Earth’s moon; dwarf planets such as Pluto and Ceres; asteroids; comets and meteoroids Sun – A sta ...
Sem one 2011 review KEY
Sem one 2011 review KEY

... the day change from season to season. 39. The constellation’s locations are very predictable, with little change from day to day. Planets, on the other hand, seem to change location at a much greater rate. How do you explain this weird truth? They are much closer to us, so small movements are easier ...
1. In Ptolemy`s geocentric model, the planet`s mo
1. In Ptolemy`s geocentric model, the planet`s mo

... distance to a planet from observing its period of rotation on its axis. 12. According to Newton's first law an object traveling in a circle does not have a force acting on it. 13. According to Newton's second law, if you double the force acting on a body, the acceleration will double. 14. Compared t ...
CopernicanRev1
CopernicanRev1

... the planets is because, being fixed in their own circles or in their own spheres whose movements they follow, they are carried across the zodiac, just as Pythagoras had first understood it, by a regulated simple and equal revolution but which results by combination in a movement that appears variabl ...
Pocket Solar System Activity
Pocket Solar System Activity

... huge size differences involved. This is a simple little model to give you an overview of the distances between the orbits of the planets and other objects in our solar system. (It is also a good tool for reviewing fractions.) Materials needed:  At least 1 meter of paper tape per person, such as add ...
Week 2 File
Week 2 File

... astronomical  observa8ons.  Some  of  these  provided  direct  evidence  for     the  heliocentric  model  and  were  published  in  Siderius  Nuncius  (Starry   Messenger).   ...
AE Module 5 Presentation
AE Module 5 Presentation

... dry and barren, with no atmosphere and no liquid water. The surface is primarily rock covered with a fine layer of dust. There are many different types of rock on the Moon, but the two most common are Moon basalt and anorthosite. The Moon’s basalt is very similar to Earth’s, but contains ...
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Comparative planetary science

Comparative planetary science or comparative planetology is a branch of space science and planetary science in which different natural processes and systems are studied by their effects and phenomena on and between multiple bodies. The planetary processes in question include geology, hydrology, atmospheric physics, and interactions such as impact cratering, space weathering, and magnetospheric physics in the solar wind, and possibly biology, via astrobiology.Comparison of multiple bodies assists the researcher, if for no other reason than the Earth is far more accessible than any other body. Those distant bodies may then be evaluated in the context of processes already characterized on Earth. Conversely, other bodies (including extrasolar ones) may provide additional examples, edge cases, and counterexamples to earthbound processes; without a greater context, studying these phenomena in relation to Earth alone may result in low sample sizes and observational biases.
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