The 8 Planets Series: The Finale

For the last few months, if you stayed tuned to my “8 Planets” series, I updated information on each of the planets and major moons, taking you on a journey through the solar system. From Mercury to Neptune, the solar system holds many wonders, twists and turns, and bizarre objects. Coincidentally, the 8 posts, corresponding to each of the planets, was spaced out on the calendar roughly relative to the distances between the planets. The four terrestrial planets, Mercury, Venus, Earth, and Mars, are relatively close to one another (less than 1 AU). These four posts were published around the same time. However, for the gaseous planets, Jupiter, Saturn, Uranus, and Neptune, posts were spread out across months to correlate with these planets’ large distances from one another. Well, thank you for tuning in! To celebrate the “8 Planets” series I created a solar system mobile, as shown below. Enjoy! The next series will be “Astronomy and Mythology: The Naming of Celestial Objects.”
Advertisements

The 8 Planets – Part 1: Mercury

NEXT STOP: MERCURY!

Mercury

What comes to mind when you think about Mercury? Perhaps the poisonous silvery liquid in old thermometers or the Roman counterpart of the Greek messenger god Hermes? The first planet of the solar system? The Moon’s look-alike? Or maybe… all of the above!

The innermost and terrestrial planet, Mercury is closest to the Sun and feels more of the Sun’s gravity than any other planet. Discovered as early as the 14th century BC, Mercury is one of the ancient planets. Mercury, like the speedy Roman messenger god, is also the speediest planet, traveling on the most elliptical (eccentric) orbit of the 8 planets. As the smallest planet, Mercury has the weakest gravity and no moons. With its heavily cratered surface, Mercury easily looks similar to Earth’s Moon and has been geologically inactive for billions of years. Its negligible atmosphere offers little resistance and protections against onslaughts of meteors and asteroids. Surprisingly, Mercury is not the hottest planet of the solar system even though it is closest to the Sun, because its very thin atmosphere cannot trap much heat. Moreover, Mercury has a low albedo (not very reflective) since its atmosphere mostly absorbs rather than reflects light from the Sun. Consequently, the Sun’s light obscures the already dim Mercury from our view, but individuals usually observe Mercury at dawn or dusk during minimal sunlight— hence, the terms morning star and evening star. Mercury’s largest surface feature is the 4,000-mile Caloris Basin, one of ~15 impact craters. Near the Caloris Basin is a region of hilly terrain called the “Weird Terrain.” Mercury has large ridges up to several hundred kilometers high on its surface. Other features are smooth plains and compression folds (rupes). Mercury’s core is large and rich in iron, since its gravity is not as strong as larger planets to compress it. It is 70% metallic and 30% silicate material. Around the now-believed-to-be molten core is the 500-700 km thick mantle and a 100-300 km think crust. In addition, due to its slow rotational period and small size, Mercury has a significant magnetic field, about 1.1% as strong as Earth’s. Like, Venus, Mercury appears in phases when observing from Earth. On average, Mercury is the closest planet to Earth at 1.08 AU (Earth to Venus is 1.3 AU).

HOW DID MERCURY FORM? – 3 Hypotheses

  1. Mercury was struck by a planetesimal 1/6 the mass of the planet and several kilometers across. The collision destroyed most of the crust and mantle, leaving a large core.
  2. Mercury was formed by the solar nebula (a gaseous cloud from which the Sun and planets formed by condensation) before the Sun’s energy output stabilized. Temperatures during the formation could have been as low as 2,500 K – 3,000 K or as high as 10,000 K. Originally twice the size as it is now, the protosun’s contraction high temperatures vaporized the outer layers of rock on Mercury.
  3. The solar nebula caused drag on materials accreting into Mercury, so that light elements left and heavier elements remained.

* MESSENGER found higher levels of potassium and sulfur than previously thought on Mercury’s surface. This means hypotheses 1 and 2 are unlikely, thus favoring the third hypothesis.

MISSIONS: MESSENGER, Mariner 10, BepiColombo

OVERVIEW

  • Order in Solar System: #1
  • Number of Moons: 0
  • Orbital Period: 88 days
  • Rotational Period: 59 days
  • Mass: 3.3 x 10^23 kg (0.055 Earths)
  • Volume: 6.083 x 10^10 km³ (0.056 Earths)
  • Radius: 2,439 km (0.3829 Earths)
  • Surface Area: 7.48 x 10^7 km² (0.147 Earths)
  • Density: 5.427 g/cm
  • Surface Pressure: trace
  • Eccentricity of Orbit: 0.2
  • Surface Temperature (Average): 340 K
  • Escape Velocity: 4.25 km/s
  • Apparent Magnitude: -2.6 to 5.7

Pyramids, Planets: Alignment!

Giza pyramids and the three planets (Mercury, Venus, Saturn) aligned

On December 3, 2012, the planets Mercury, Venus, and Saturn will align with the Giza Pyramids in Egypt. This will be the first planetary/pyramid alignment in 2,737 years! Now, the three Giza pyramids are also in perfect alignment with the three stars of Orion’s belt. In 1983, Robert Bauval proposed this Orion correlation theory and published this idea in Discussions in Egyptology in 1989. The Giza pyramids were built in the 3rd millennium B.C. The alignment is very curious. Could the Egyptians have built the Giza pyramids that way on purpose?

Giza pyramids and Orion’s Belt aligned

The Solar System: Basics

The Solar System

COMPARATIVE PLANETOLOGY

  • Eccentricity of Orbit: measures the ellipticity of orbit (ranges 0-1, with 0 as spherical and 1 as very elliptical)
  • Density: mass per unit volume; mass in grams and volume in cubic centimeters
  • Oblateness: measures how much the middle section of the planet bulges
  • Surface Gravity: the larger the surface gravity, the thicker the atmosphere as gravity pulls in more gases
  • Albedo: measures the fraction of light reflected compared to the amount of light received from the Sun; the higher the albedo, the more reflective the surface
  • Escape Velocity: minimum speed or velocity needed to escape the planet’s gravitational pull
  • Rotation: most planets rotate in counter-clockwise direction (prograde); others rotate in the clockwise direction (retrograde)
    • Rotational period is shortest for gaseous planets and longest for Venus
  • Roche Limit: about two and a half times the radius of the planet; within the Roche Limit, matter cannot accretes to form moons because the tidal force of the planet tears matter apart to form rings

Giant Planets: Giant planets have lighter elements such as hydrogen and helium in their atmospheres. They have stronger gravity and are at larger distances from the Sun. Jupiter, Saturn, and Neptune are stormy with great spots of lasting storms and belts and zones. However, Uranus is comparatively bland and uniform. All giant planets are home to convection, or hot gases rising and cold gases falling.

Terrestrial Planets: Terrestrial planets have heavier elements such as carbon, oxygen, and nitrogen. Mercury is most heavily cratered while Earth is least cratered. Larger terrestrial planets have plate tectonics. Earth has a sizable magnetic fields that can protect it from solar wind particles and Van Allen Belts. Earth has the “Goldilocks phenomenon,” or the right conditions for the development of life.

For more information: THE SUN, THE PLANETS, PLANETESIMALS

The Planets: Part I

“The Planets” sub-page under the “The Solar System” page has now been complete and updated with pictures and additional information. Part I includes the terrestrial planets: Mercury, Venus, Earth, and Mars! See the page here.