Vocabulary Flashcards
Perihelion
closest approach to the sun
Aphelion
Furthest point from the sun
Trojan
a trojan is a small celestial body (mostly asteroids) that shares the orbit of a larger one, remaining in a stable orbit approximately 60° ahead of or behind the main body near one of its Lagrangian points L4 and L5. Trojans can share the orbits of planets or of large moons.
Kirkwood gaps
Kirkwood gap is a gap or dip in the distribution of the semi-major axes (or equivalently of the orbital periods) of the orbits of main-belt asteroids. They correspond to the locations of orbital resonances with Jupiter.
Lagrange points
Lagrange points are positions in space where objects sent there tend to stay put. At Lagrange points, the gravitational pull of two large masses precisely equals the centripetal force required for a small object to move with them. These points in space can be used by spacecraft to reduce fuel consumption needed to remain in position.
Refractory group
High melting points, low vapor pressures
Troilite
FeS
Iron Sulphite
Chondrite
A chondrite is a stony (non-metallic) meteorite that has not been modified, by either melting or differentiation of the parent body. They are formed when various types of dust and small grains in the early Solar System accreted to form primitive asteroids.
3 Asteroid types
C-Type - Carbonaceous/Carbon-rich
M-Type - Metallic
S-Type - Sillicate
Achondrite
An achondrite is a stony meteorite that does not contain chondrules. It consists of material similar to terrestrial basalts or plutonic rocks and has been differentiated due to melting and recrystallization on or within parent bodies.
Meteorite Falls (NOT finds) distribution
Chondrites 86%
Achondites 9%
Irons 4%
Stony Irons 1%
4 Achondrite Categories
Primitive (0.3)
Asteroidal (8)
Martian (0.5)
Lunar (rare)
Main group of asteroidal achondrites
HED
Howardites, Eucrities, Diogenites
May originate from Vespa
Milankovitch Insolation Cycles
3 factors
The Milankovitch cycles include:
The shape of Earth’s orbit, eccentricity;
The angle Earth’s axis is tilted with respect to Earth’s orbital plane, obliquity
The direction Earth’s axis of rotation is pointed, precession
Field of view
Area that can be photographed in one go.
FOV = 2D x tan(θ/2)