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Lintang is a state constituency in Perak, Malaysia, that has been represented in the Perak State Legislative Assembly. Demographics. Ethnic breakdown of Lintang's ...
Batu Lintang is a state constituency in Sarawak, Malaysia, that has been represented in the Sarawak State Legislative Assembly since 1991.. The state constituency was created in the 1987 redistribution and is mandated to return a single member to the Sarawak State Legislative Assembly under the first past the post voting system.
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 ...
The physics convention.Spherical coordinates (r, θ, φ) as commonly used: (ISO 80000-2:2019): radial distance r (slant distance to origin), polar angle θ (angle with respect to positive polar axis), and azimuthal angle φ (angle of rotation from the initial meridian plane).
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.
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.
The Behrmann projection with Tissot's indicatrices The Mercator projection with Tissot's indicatrices. In cartography, a Tissot's indicatrix (Tissot indicatrix, Tissot's ellipse, Tissot ellipse, ellipse of distortion) (plural: "Tissot's indicatrices") is a mathematical contrivance presented by French mathematician Nicolas Auguste Tissot in 1859 and 1871 in order to characterize local ...
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.