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scicreat2
scicreat2

... Earth, moon and planets each created for a specific purpose, each with a distinctive composition and structure Only the earth would be found to have a hydrosphere capable of supporting life Only the earth would be found to have an atmosphere capable of supporting life Evidence of decay and catastrop ...
Chapter 11b: Cloud-Covered Venus PowerPoint
Chapter 11b: Cloud-Covered Venus PowerPoint

... Venus is the second planet from the Sun Venus is the second largest terrestrial planet Venus has many active volcanoes Venus is almost a twin of the Earth except … – Venus has ~ 93 times Earth’s atmosphere – Venus’ atmosphere is ~ 96% CO2 – Venus is perpetually cloud covered – Venus’ average surface ...
11b. Cloud-Covered Venus Venus Data (Table 11
11b. Cloud-Covered Venus Venus Data (Table 11

... Venus is the second planet from the Sun Venus is the second largest terrestrial planet Venus has many active volcanoes Venus is almost a twin of the Earth except … –  Venus has ~ 93 times Earth’s atmosphere –  Venus’ atmosphere is ~ 96% CO2 –  Venus is perpetually cloud covered –  Venus’ average sur ...
Basaltic volcanism on the terrestrial planets: a window to planetary
Basaltic volcanism on the terrestrial planets: a window to planetary

... In fact, this is the main factor of crust formation, differentiation and geological processing of the terrestrial planets and the differentiated asteroids. Astronomical observations have ascertained the presence of volcanic plains, most probably basaltic lava flows on the surfaces of terrestrial pla ...
challenger center simulators
challenger center simulators

... Scene 11 (Earth time lapse {old Scene 21}) The last time the sun was where it is now, Earth had but one continent … and dinosaurs roamed the land. Scene 12 (Solar birth {Old Scene 2 – first 43 seconds}) But using supercomputers and through studying other stars, we can travel, as if in a time machine ...
Section 2 Practice Test
Section 2 Practice Test

... ____ 12. Why are the inner planets called terrestrial planets? a. because they are very hot c. because most are gas giants b. because they resemble Earth d. because they can support life ____ 13. What is one way that gas giants differ from the terrestrial planets? a. They are much smaller. c. Their ...
Where to Look For Life? - Journey through the Universe
Where to Look For Life? - Journey through the Universe

... variations. If sunlight falls on an object in space, it heats up quickly, but if the object is then shaded from sunlight, it cools off just as quickly. This means that if a planet has no atmosphere, a given point on the planet’s surface can see extreme variation in temperatures between day (when the ...
THE CONTRIBUTIONS OF COMETS TO
THE CONTRIBUTIONS OF COMETS TO

... Icy planetesimals also originated in the subnebulae surrounding the giant planets at the time they formed. Some of these accreted to form the icy satellites; others crashed into the forming planets, and still others could have been scattered into the Oort cloud. Finally, several objects in the outer ...
Gravity and Orbits Scripted - UTeach Ideas
Gravity and Orbits Scripted - UTeach Ideas

... http://en.wikipedia.org/wiki/File:GPS_Satellite_NASA_art-iif.jpg ...
The Solar System
The Solar System

... Figure 1.7 shows the relative sizes of the orbits of the planets, asteroid belt, and Kuiper belt. In general, the farther away from the Sun, the greater the distance from one planet’s orbit to the next. The orbits of the planets are not circular but slightly elliptical, with the Sun located at one o ...
Pluto
Pluto

... In late 2005, two additional tiny moons were found to orbit Pluto (known as Nix and Hydra). They are estimated to be between 60 and 200 km in diameter Pluto's orbit is highly eccentric. At times it is closer to the Sun than Neptune (as it was from January 1979 thru February 11 1999) Pluto rotates in ...
assigned - subfreshmanhomework2016-2017
assigned - subfreshmanhomework2016-2017

... The Engage phase is meant to capture your attention. The What Do You See? picture in each section has been drawn by Tomas Bunk. Tomas Bunk is not a scientist but a well-recognized cartoonist. He uses his artistic talent and enjoys drawing humorous illustrations that show real Earth and space science ...
EarthComm_c1s1
EarthComm_c1s1

... The Engage phase is meant to capture your attention. The What Do You See? picture in each section has been drawn by Tomas Bunk. Tomas Bunk is not a scientist but a well-recognized cartoonist. He uses his artistic talent and enjoys drawing humorous illustrations that show real Earth and space science ...
parte ii - NivelesDeIngles
parte ii - NivelesDeIngles

... they may be called plutons. Shows a dome–shaped or large dome. Over 100 km, if less is called Stock. Its composition is quite homogeneous, generally made of granite or granodiorite (combination of granite and diorite). Big Bang – Big Bang – (astr.) The Big Bang model is the prevailing cosmologicalth ...
Scientific Justification
Scientific Justification

... Using a 1D MHD model one can extrapolate solar wind measurements made near the Earth out to Jupiter and Saturn. The extrapolation model (led by K.C. Hansen) is very high resolution in radius, with an assumed spherical symmetry of the solar corona and solar wind. If the Sun is in a highly dynamic sta ...
Moon - mrnicholsscience
Moon - mrnicholsscience

... From near to far, from here to there, funny things are everywhere (TSG 1960) ...
Characterizing the purple Earth: Modelling the globally
Characterizing the purple Earth: Modelling the globally

... one of the observational approaches used for this purpose, providing a tool to study the spectrum of Earth in the visible (e.g. Goode et al. 2001; Woolf et al. 2002; Qiu et al. 2003; Pallé et al. 2003, 2004), and also in the near-infrared (Turnbull et al. 2006; Pallé et al. 2009) and in the near-U ...
Moons in our Solar System
Moons in our Solar System

... synchronous orbit, meaning they always show the same face to each other For the Greeks, Charon was the boatman who carried dead souls to the underworld, ruled by Pluto Pluto ...
The Solar System
The Solar System

... observations of bodies in our solar system. 2. A year is the time it takes for the Earth to orbit the sun; year = revolution. 3. A month is the time it takes for the moon to orbit the Earth. ...
INPOP06. A new numerical planetary ephemeris
INPOP06. A new numerical planetary ephemeris

... paleoclimate studies of the Earth and Mars over several millions of years. Indeed, because of the chaotic behavior of the orbital solutions of the Solar System (Laskar, 1989, 1990), extending the astronomical solutions from 40 Myr (Laskar et al. 2004a,b) to 60 Myr, corresponds to a gain of two order ...
Science Notebook Masters
Science Notebook Masters

... 1. What is soil made of? 2. What are the two most important properties of soil? 3. Which soil is best for plants and why: sandy soil, clay soil, or a mixture of sand and clay in the soil? 4. How do animals living in soil help make the soil better for growing plants? 5. What are the two ways the ...
SRMP Solar System Curriculum - American Museum of Natural History
SRMP Solar System Curriculum - American Museum of Natural History

... recording the moons of Jupiter. His daily record allowed for the determination of the timing of the orbits, and is not trivial without a computer. Hand out a Moons of Jupiter sheet to all students along with colored pencils or markers. Explain that this is a simulation of Galileo’s data. (In fact, t ...
Lecture 15: Small Solar System Bodies
Lecture 15: Small Solar System Bodies

... gravity strongly perturbed the orbits of almost all the asteroids •  Most of them got nudged into highly eccentric orbits, from which they either leave the Solar System or head inwards toward the Sun •  A fraction of the asteroids headed inwards may have hit the early Earth! Page 13 ...
Document
Document

... planets. Specifically, the dust could be more efficient than larger bodies in delivery of organic (prebiogenic) or even biogenic matter to the planets. • This is explained by the fact that dust particles are not subjected to intense heating (usually higher than 100-150 C) when they enter the atmosph ...
HS The Solar System
HS The Solar System

... Greeks identified five of the planets and for many centuries they were the only planets known. Since then, scientists have discovered two more planets, many other solar-system objects and even planets found outside our solar system. ...
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Earth's rotation



Earth's rotation is the rotation of the planet Earth around its own axis. The Earth rotates from the west towards east. As viewed from North Star or polestar Polaris, the Earth turns counter-clockwise.The North Pole, also known as the Geographic North Pole or Terrestrial North Pole, is the point in the Northern Hemisphere where the Earth's axis of rotation meets its surface. This point is distinct from the Earth's North Magnetic Pole. The South Pole is the other point where the Earth's axis of rotation intersects its surface, in Antarctica.The Earth rotates once in about 24 hours with respect to the sun and once every 23 hours 56 minutes and 4 seconds with respect to the stars (see below). Earth's rotation is slowing slightly with time; thus, a day was shorter in the past. This is due to the tidal effects the Moon has on Earth's rotation. Atomic clocks show that a modern-day is longer by about 1.7 milliseconds than a century ago, slowly increasing the rate at which UTC is adjusted by leap seconds.
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