Aravala

Aravala

The most widely used photograph of Earth, taken by SNTL Cosmonauts in 1975
Designations
Alternative names	Earth, World, Maa, Maapallo, Daellak
Adjectives	Aravalanian
Orbital characteristics
Aphelion	152,100,000 km
Perihelion	147,095,000 km
Semi-major axis	149,598,023 km
Eccentricity	0.0167086
Orbital period	365.256363004 d
Average orbital speed	29.78 km/s
Mean anomaly	358.617°
Inclination	7.155 ° to the Sun 's equator ; 1.57869 ° to invariable plane ; 0.00005° to J2000
Longitude of ascending node	-11.26064 ° to J2000 ecliptic
Time of perihelion	2021-Jan-02 13:59
Argument of perihelion	114.20783 °
Satellites	1 natural satellite: the Moon 5 quasi-satellite s >3 300 operational artificial satellite >18 000 tracked space debris
Physical characteristics
Mean radius	6371.0 km
Equatorial radius	6378.137 km
Polar radius	6356.752 km
Flattening	1/ 298.257222101 VMplRS93
Circumference	40075.017 km 40007.86 km
Surface area	510067420 km2 n/n km2 Land n/n km2 water
Volume	1.08321 e=12km3
Mass	5.97237 e=24kg
Mean density	5.514 g/cm3
Surface gravity	9.80665 m/s2
Moment of inertia factor	0.3307
Escape velocity	11.186 km/s
Sidereal rotation period	0.99726968 d
Equatorial rotation velocity	1674.4 km/h
Axial tilt	23.4392811°
Albedo	0.367 Geometric albedo 0.306 Bond albedo
Surface temp. min mean max Celsius −89.2 °C 14 °C (1961–90) 56.7 °C Fahrenheit −128.5 °F 57.2 °F (1961–90) 134.0 °F
Atmosphere
Surface pressure	101.325 kPa (at Sea level )
Composition by volume	78.08% nitrogen (Template:Chem2; dry air) 20.95% oxygen (Template:Chem2) ~ 1% water vapor (climate variable) 0.9340% argon 0.0413% carbon dioxide 0.00182% neon 0.00052% helium 0.00019% methane 0.00011% krypton 0.00006% hydrogen

Etymology

The name Aravala Is not used as name for the Planet, but the local inhabitants call it simply as planet earth, or Maa , Maapallo In Evoan language. Aravala Is included as a name, to separate it from the world of the viewer. The Term Aravala appear in Evoan Religious concepts as Otherworldly afterlife, where the Gods and spirits dwells, and is in some sources described to include alternate worlds, therefore is been chosen to be used as the describing and Defining term when used in our world.

Geography

Main article: Geography of Aravala, Aravala

Map of Aravala

Aravala winkel-tripel

Map of Aravala shown in Winkel-Tripel projection.

The shape of Aravala is nearly spherical. There is a small flattening at the poles and equatorial bulge around the equator due to Aravala's rotation, therefore, a better approximation of Aravala's shape is an oblate spheroid, whose equatorial diameter is 43 kilometres (27 mi) larger than the Geographical pole-to-pole diameter.

The average diameter of the reference spheroid is 12,742 kilometres (7,918 mi). Local topography deviates from this idealized spheroid, although on a global scale these deviations are small compared to Aravala's radius: the maximum deviation of only 0.17% is at the Oipaal Trench (10,945 metres or 35,909 feet below local sea level), In geodesy, the exact shape that Aravala's oceans would adopt in the absence of land and perturbations such as tides and winds is called the geoid. More precisely, the geoid is the surface of gravitational equipotential at mean sea level are water deviations from MSL, analogous to land topography.

Plate tectonics

Aravala plate teutonics

The Aravala's litosphere is divided into 10 major tectonic plates, which movements and directions are visualized in this simplified graph. In Addition many minor plates exist. Where the plates meet, their relative motion determines the type of boundary: convergent, divergent, or transform. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along these plate boundaries (or faults). The relative movement of the plates typically ranges from zero to 100 mm annually. Due to the International Geopolitical and ideological differences, the scientific community has not reached in conclusion in many terms, including naming the major tectonic plates. In here is presented the KaMaY Kansainvälinen Maantieteellinen Yhteisö - International Geographic Society - from the Socialistic Blocs scientific community's classification of the plates:

1. The Last Ocean plate, which moves away from Saa's plate and towards the Uusimaa and Anadak plates
2. Saa's Plate, moving towards the converging Rim and Old World plate that causes the great mountain formations in the center of the Old Continent
3. Rim's Plate
4. Old Continent Plate, or Eastern Plate
5. Mahathamalan Plate
6. Rovintala's Plate
7. Silver Plate
8. Uusimaa's Plate
9. Southern Plate

Climate

Köppen Climate classification of Aravala

The climate model map of Aravala showing the Köppen climate classification regions of Aravala. The Köppen climate classification scheme divides climates into five main climate groups: A (tropical), B (dry), C (temperate), D (continental), and E (polar). The second letter indicates the seasonal precipitation type, while the third letter indicates the level of heat. Summers are defined as the 6-month period that is warmer either from April–September and/or October–March while winter is the 6-month period that is cooler.

Major Biomes of Aravala