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English: This drawing/sketchup shows the most important terms related to the basketball court: Corner, Short Corner, Low Post, Block, Restricted area, Wing, High Post ...
The home court of the Miami Heat of the National Basketball Association. In basketball, the basketball court is the playing surface, consisting of a rectangular floor, with baskets at each end. Indoor basketball courts are almost always made of polished wood, usually maple, with 10 feet (3.048 m)-high
Basketball court: Date: 20 January 2007, 12:36 (UTC) Source: modification of Basketball court dimensions.png: Author: maix ¿? Permission (Reusing this file) public domain with ShareAlike (license used for modifications must allow editing) Other versions: Basketball court dimensions.png, Basketball court dimensions.svg
Basketball court: Date: 21 January 2007, 13:27 (UTC) Source: modification of Basketball court dimensions.png: Author: maix ¿? Permission (Reusing this file) public domain with ShareAlike (license used for modifications must allow editing) Other versions: Basketball court dimensions.png Image:Basketball court dimensions no label.svg
This image is a derivative work of the following images: File:Basketball_court.png licensed with Cc-by-sa-3.0,2.5,2.0,1.0, GFDL . 2008-06-21T11:09:11Z Pacoperez6 1600x2203 (180065 Bytes) {{Information |Description={{en|Diagram of a basketball court used primarily for men showing: *Top half **FIBA, NBA and NCAA (men) markings **Measurements for FIBA three-point line and base of the key.
Mechanically, it can be divided into lithosphere, asthenosphere, mesospheric mantle, outer core, and the inner core. Chemically, Earth can be divided into the crust, upper mantle, lower mantle, outer core, and inner core. [6] The geologic component layers of Earth are at increasing depths below the surface. [6]: 146
The asthenosphere (from Ancient Greek ἀσθενός (asthenós) 'without strength') is the mechanically weak [1] and ductile region of the upper mantle of Earth. It lies below the lithosphere , at a depth between c. 80 and 200 km (50 and 120 mi) below the surface, and extends as deep as 700 km (430 mi).
The lithosphere–asthenosphere boundary (referred to as the LAB by geophysicists) represents a mechanical difference between layers in Earth's inner structure. Earth's inner structure can be described both chemically ( crust , mantle , and core ) and mechanically.