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  2. Latitude - Wikipedia

    en.wikipedia.org/wiki/Latitude

    Two levels of abstraction are employed in the definitions of latitude and longitude. In the first step the physical surface is modeled by the geoid, a surface which approximates the mean sea level over the oceans and its continuation under the land masses.

  3. Kármán line - Wikipedia

    en.wikipedia.org/wiki/Kármán_line

    Earth's atmosphere photographed from the International Space Station.The orange and green line of airglow is at roughly the altitude of the Kármán line. [1]The Kármán line (or von Kármán line / v ɒ n ˈ k ɑːr m ɑː n /) [2] is a conventional definition of the edge of space; it is widely but not universally accepted.

  4. List of national capitals by latitude - Wikipedia

    en.wikipedia.org/wiki/List_of_national_capitals...

    Latitude ("−" indicates southern hemi-sphere) City Country Notes −0.25 Quito: Ecuador: Highest official capital. 0.3 Kampala: Uganda: 0.33 São Tomé

  5. Antipodes - Wikipedia

    en.wikipedia.org/wiki/Antipodes

    In geography, the antipode (/ ˈ æ n t ɪ ˌ p oʊ d, æ n ˈ t ɪ p ə d i /) of any spot on Earth is the point on Earth's surface diametrically opposite to it. A pair of points antipodal (/ æ n ˈ t ɪ p ə d əl /) to each other are situated such that a straight line connecting the two would pass through Earth's center.

  6. Fault (geology) - Wikipedia

    en.wikipedia.org/wiki/Fault_(geology)

    Satellite image of a fault in the Taklamakan Desert.The two colorful ridges (at bottom left and top right) used to form a single continuous line, but have been split apart by movement along the fault.

  7. Kyrgyzstan - Wikipedia

    en.wikipedia.org/wiki/Kyrgyzstan

    Kyrgyzstan, [a] officially the Kyrgyz Republic, [b] [12] is a landlocked country in Central Asia, lying in the Tian Shan and Pamir mountain ranges. Bishkek is the capital and largest city.

  8. Continental crust - Wikipedia

    en.wikipedia.org/wiki/Continental_crust

    The thickness of Earth's crust (km). The continental crust consists of various layers, with a bulk composition that is intermediate (SiO 2 wt% = 60.6). [5] The average density of the continental crust is about, 2.83 g/cm 3 (0.102 lb/cu in), [6] less dense than the ultramafic material that makes up the mantle, which has a density of around 3.3 g/cm 3 (0.12 lb/cu in).

  9. Lintang - Wikipedia

    en.wikipedia.org/wiki/Lintang

    Lintang may be, Lintang language; Kampung Lintang This page was last edited on 28 January 2019, at 07:22 (UTC). Text is available under the Creative Commons ...