Mas punya peta kontur, hidrologi, klimatologi, peta banjir, topografi jakarta ga??pokoknya yg berhubungan dg aspek fisik dasar. Thanks ya mas.q berharap yg ga pake beli.coz masih mahasiswa.oke thanks. Cinema 4d download windows 10. Peta topografi adalah jenis peta yang ditandai dengan skala besar dan detail, biasanya menggunakan garis kontur dalam pemetaan modern. Sebuah peta topografi biasanya terdiri dari dua atau lebih peta yang tergabung untuk membentuk keseluruhan peta. Sebuah garis kontur merupakan kombinasi dari.

Contains map data © contributors, made available under the terms of the. The ODbL does not require any particular license for maps produced from ODbL data; map tiles produced by the OpenStreetMap foundation are licensed under the, but maps produced by other people may be subject to other licences. Open Database License ODbL true Geotemporal data Map projection Transverse Mercator Zona 47 N Heading Bounding box N: 1.733161°N W: 96.886798°E E: 98.133142°E S: 0.466788°N Georeferencing If inappropriate please set warp_status=skip to hide.

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A contour line (also isoline, isopleth, or isarithm) of a function of two variables is a curve along which the function has a constant value. In cartography, a contour line (often just called a 'contour') joins points of equal elevation (height) above a given level, such as mean sea level.

A contour map is a map illustrated with contour lines, for example a topographic map, which thus shows valleys and hills, and the steepness of slopes. The contour interval of a contour map is the difference in elevation between successive contour lines. Contour lines are curved, straight or a mixture of both lines on a map describing the intersection of a real or hypothetical surface with one or more horizontal planes.

H 264 progdvb pack download. The configuration of these contours allows map readers to infer relative gradient of a parameter and estimate that parameter at specific places. Contour lines may be either traced on a visible three-dimensional model of the surface, as when a photogrammetrist viewing a stereo-model plots elevation contours, or interpolated from estimated surface elevations, as when a computer program threads contours through a network of observation points of area centroids. In the latter case, the method of interpolation affects the reliability of individual isolines and their portrayal of slope, pits and peaks.