Difference between revisions of "Aravala"

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  | {{convert|361132000|km2|mi2|comma=gaps|abbr=on|disp=x| water <small>(|)</small>}}
 
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| volume  = [[Volume of the Earth|{{val|1.08321|e=12|u=km3}}]]  
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| volume  = [[Volume of the Earth|{{val|1.08321|e=12|u=km3}}]] <small>({{val|2.59876|e=11|u=cu mi}})</small><ref name="earth_fact_sheet" />
 
| mass    = {{val|5.97237|e=24|u=kg}} <small>({{val|1.31668|e=25|u=lb}})</small><ref name="Luzum2011" /> <br /> <small>({{val|3.0|e=-6|ul=solar mass}})</small>
 
| mass    = {{val|5.97237|e=24|u=kg}} <small>({{val|1.31668|e=25|u=lb}})</small><ref name="Luzum2011" /> <br /> <small>({{val|3.0|e=-6|ul=solar mass}})</small>
 
| density  = {{convert|5.514|g/cm3|lb/cuin|comma=gaps|abbr=on|disp=x| <small>(|)</small>}}<ref name="earth_fact_sheet" />
 
| density  = {{convert|5.514|g/cm3|lb/cuin|comma=gaps|abbr=on|disp=x| <small>(|)</small>}}<ref name="earth_fact_sheet" />

Revision as of 17:41, 15 May 2021

Aravala Astronomical symbol of Earth
Drawing of Aravala, after the famous picture by SNTL Cosmonauts in 1975 Showing the Centrall Archipelago in the middle and the Old Continent on the left, and the Newland in the far right.
The most widely used photograph of Earth, taken by SNTL Cosmonauts in 1975
Designations
Earth, World, Maa, Maapallo, Daellak
Adjectives Aravalanian
Orbital characteristics
Aphelion 152,100,000 km
Perihelion 147,095,000 km
149,598,023 km
Eccentricity 0.0167086
365.256363004 d
29.78 km/s
358.617°
Inclination 7.155 ° to the Sun 's equator ; 1.57869 ° to invariable plane ; 0.00005° to J2000
-11.26064 ° to J2000 ecliptic
2021-Jan-02 13:59
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
  • 510067420 km2 (196938130 sq mi)[1][n 1]
  • 148940000 km2 land (57510000 sq mi)
  • 361132000 km2 water (139434000 sq mi)
Volume [[Volume of the Earth|Template:Val]] (Template:Val)[2]
Mass Template:Val (Template:Val)[3]
(Template:Val)
Mean density
 5.514 g/cm3 (0.1992 lb/cu in)[2]
9.80665 m/s2 ([[Gravity of Earth|Template:Val]]; 32.1740 ft/s2)[4]
0.3307[5]
11.186 km/s[2] (40270 km/h; 25020 mph)
Template:Val[6]
(23h 56m 4.100s)
Equatorial rotation velocity
 1674.4 km/h[7]
(0.4651 km/s; 1674.4 km/h; 1040.4 mph)
Template:Val[8]
Albedo Template:Ublist
Surface temp. min mean max
Celsius −89.2 °C[9] 14 °C (1961–90)[10] 56.7 °C[11]
Fahrenheit −128.5 °F 57.2 °F (1961–90) 134.0 °F
Atmosphere
Surface pressure
 Template:Val (at MSL)
Composition by volume


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 teutonics

Climate

Continents

  1. ↑ Cite error: Invalid <ref> tag; no text was provided for refs named Pidwirny_2006_8
  2. ↑ 2.0 2.1 2.2 2.3 2.4 Cite error: Invalid <ref> tag; no text was provided for refs named earth_fact_sheet
  3. ↑ Cite error: Invalid <ref> tag; no text was provided for refs named Luzum2011
  4. ↑ Cite error: Invalid <ref> tag; no text was provided for refs named NIST2008
  5. ↑ Cite error: Invalid <ref> tag; no text was provided for refs named Williams1994
  6. ↑ Cite error: Invalid <ref> tag; no text was provided for refs named Allen296
  7. ↑ Cite error: Invalid <ref> tag; no text was provided for refs named Cox2000
  8. ↑ Cite error: Invalid <ref> tag; no text was provided for refs named IERS
  9. ↑ Cite error: Invalid <ref> tag; no text was provided for refs named asu_lowest_temp
  10. ↑ Template:Cite journal
  11. ↑ Cite error: Invalid <ref> tag; no text was provided for refs named asu_highest_temp
  12. ↑ "Trends in Atmospheric Carbon Dioxide: Recent Global [[:Template:Chem2]] Trend". Earth System Research Laboratory. National Oceanic and Atmospheric Administration. 19 October 2020. Archived from the original on 4 October 2020.  Unknown parameter |url-status= ignored (help); URL–wikilink conflict (help)


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