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Tag Archives: blog7
Uranus
Uranus the most mysterious of the gas giants, in its form, orbit, and rotation. It is a widely known fact that Uranus rotates on its side, but its strange tilt also means that its magnetic field is skewed, so that its magnetic north and south are vastly different than its polar. In addition, the storms… Continue reading
Comets and stuff
For blog 7 I’ve decided to write about comets. Comets, according to space.com is “an icy body that releases gas or dust”(space.com) Astronomers believe that comets are leftovers of the gas, dust, ice, and rocks that originally formed our solar system. It is believed that comets carried some of the water and organic molecules that […] Continue reading
Stop! In the Name of…
Gravity? What causes Hot Jupiters to not be eaten by their parent stars? Continue reading
Extrasolar planets
image source In the class, we learn about the astrometric technique, Doppler technique and direct imaging used to detect extrasolar planets. And in this blog, I’d like to introduce some other planet-hunting strategies that have proved to be applicable. The first method is called gravitational microlensing. A gravitational microlensing occurs only when two stars are […] Continue reading
Extrasolar planets
image source In the class, we learn about the astrometric technique, Doppler technique and direct imaging used to detect extrasolar planets. And in this blog, I’d like to introduce some other planet-hunting strategies that have proved to be applicable. The first method is called gravitational microlensing. A gravitational microlensing occurs only when two stars are […] Continue reading
Halley’s Comet
Halley’s Comet is visible from Earth every 75-76 years. It is the only known short-period comet (a comet that has an orbital period of less than 200 years) that is visible to the naked eye. Halley most recently visited the inner parts … Continue reading → Continue reading
Posted in Class, Small SS Objects, SolarSystem
Tagged astro2110, blog7, comet
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Pluto – A Dwarf Planet
Pluto is a Dwarf planet in the ring of objects beyond Neptune called the Kuiper Belt. Similar to other objects in the Kuiper Belt, Pluto is composed of rock and ice. Its orbital period is 248 Earth years, and has an inclined orbital path compared to all the planets whose paths lie in the ecliptic […] Continue reading
Creation of the Kuiper Belt
Recently in class we’ve been talking about the outer portion of our Solar System. Beyond Neptune lies the Kuiper Belt, the disc-shaped region that begins at about 30 AUs and ends around 55 AUs. The Kuiper Belt is home to hundreds of thousands of icy bodies, an estimated trillion or more comets, and Pluto, according to… More Creation of the Kuiper Belt Continue reading
Posted in Observables
Tagged astro2110, blog7, Kuiper Belt, Solar System, Uncategorized
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Volcanic Io
Volcanoes are one of the coolest geographical features of Earth (in my opinion), but volcanoes outside of our world are even cooler. Jupiter’s moon Io is the most volcanically active world in our solar system – in other words, it is FULL of volcanic awesome-ness. Io’s volcanic activity produces HUGE volcanic plumes. To give some […] Continue reading
Posted in Moons, Science
Tagged astro2110, blog7, comparison, Io, jupiter, Moon, Solar System, volcano
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A Dance to Remember
Twice now our class has been introduced to the Kepler Orrery IV model, and both times the question of why our solar system seems to be such an oddball has crossed my mind. Based on the Kepler Orrery IV model, planets much larger than Earth should be orbiting closer than the orbit of Mercury. So […] Continue reading