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Basketball court dimensions.png, Basketball court dimensions.svg I, the copyright holder of this work, hereby publish it under the following licenses: This file is licensed under Creative Commons ShareAlike 1.0 License.
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
Earth's inner structure can be described both chemically (crust, mantle, and core) and mechanically. The lithosphere–asthenosphere boundary lies between Earth's cooler, rigid lithosphere and the warmer, ductile asthenosphere. The actual depth of the boundary is still a topic of debate and study, although it is known to vary according to the ...
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 ...
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.
The pressure at the bottom of the mantle is ≈140 GPa (1.4 Matm). [24] The mantle is composed of silicate rocks richer in iron and magnesium than the overlying crust. [25] Although solid, the mantle's extremely hot silicate material can flow over very long timescales. [26] Convection of the mantle propels the motion of the tectonic plates in the
The subcontinental lithospheric mantle (SCLM) is the uppermost solid part of Earth's mantle associated with the continental lithosphere. The modern understanding of the Earth's upper mantle is that there are two distinct components - the lithospheric part and the asthenosphere .
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).