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[1] [2] [3] German sources may refer to a shield wall that protects two or more sides as a Hoher Mantel or Mantelmauer, which is variously translated as "mantle-wall", [4] "mantle wall" [5] or "high screen-wall". [6] There is often no clear, definitive distinction between a shield wall and a mantle wall.
Panels are made slightly smaller than the available space within the frame to provide room for movement. Wood will expand and contract across the grain, and a wide panel made of solid wood could change width by a half of an inch, warping the door frame. By allowing the wood panel to float, it can expand and contract without damaging the door.
Mantel—Either the shelf above a fireplace or the structure to support masonry above a fireplace [23] Smoke shelf—A shelf below the smoke chamber and behind the damper. It collects debris and water falling down the flue. [24] Throat (waist)—The narrow area above a fireplace usually where the damper is located. [21]
Airy isostasy, in which a constant-density crust floats on a higher-density mantle, and topography is determined by the thickness of the crust. Airy isostasy applied to a real-case basin scenario, where the total load on the mantle is composed by a crustal basement, lower-density sediments and overlying marine water
Plates in the crust of Earth. Earth's crust is its thick outer shell of rock, referring to less than one percent of the planet's radius and volume.It is the top component of the lithosphere, a solidified division of Earth's layers that includes the crust and the upper part of the mantle. [1]
At a subduction zone the relatively cold, dense oceanic crust sinks down into the mantle, forming the downward convecting limb of a mantle cell, which is the strongest driver of plate motion. The relative importance and interaction of other proposed factors such as active convection, upwelling inside the mantle, and tidal drag of the Moon is ...
English: Illustration of a tension leg mooring for a floating platform. Left-hand side: free-floating, cables (red) not under tension Right-hand side: cables have been tensioned ballasted floating structure (grey) underwater cables (red) connect seabed anchors (light grey) with lower legs
Crustal thickening has an upward component of motion and often occurs when continental crust is thrust onto continental crust. Basically nappes (thrust sheets) from each plate collide and begin to stack one on top of the other; evidence of this process can be seen in preserved ophiolitic nappes (preserved in the Himalayas) and in rocks with an inverted metamorphic gradient.
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