Definition, Betydelse & Anagram | Engelska ordet JOINTING

Definition av JOINTING

1. böjningsform av joint
2. presensparticip av joint

Exempel på hur man kan använda JOINTING i en mening

• One of the features of the crater is its squared-off outline, believed to be caused by existing regional jointing (cracks) in the strata at the impact site.
• The jointer plane, also known as the try plane or trying plane, is a type of hand plane used in woodworking to straighten the edges of boards in the process known as jointing, and to flatten the faces of larger boards.
• Flood basalt commonly displays columnar jointing, formed as the rock cooled and contracted after solidifying from the lava.
• The distinctive columnar jointing of the dolerite rock is the result of stresses caused by the cooling and solidifying of the melt, and there are minor crush zones associated with later compression.
• Apart from trimming and flushing, they can be used for jointing, rounding edges, chamfering, routing grooves and dados, dovetails, even mortise and tenons.
• Frequently, there is some degree of irregularity including foliation, veining, jointing, or layering that in some cases helps with soil formation and in other cases hampers it.
• In agriculture, the jointing stage is that point at which the internodal tissue in the grass leaf begins to elongate, forming a stem (culm).
• A foreman at the foundry, Thomas Gregory, drew the detailed designs for the members, resulting in the use of carpentry jointing details such as mortise and tenon joints and dovetails.
• This low viscosity resulted in emplacement as a series of lobate flows with a stacked pancake-like morphology which cooled rapidly resulting in porphyritic textures and widespread columnar jointing.
• Sedgwick investigated the phenomena of metamorphism and concretion, and was the first to distinguish clearly between stratification, jointing, and slaty cleavage.
• The jaws of Edestus were operated by a two gear system, involving double jointing of the quadrate bone allowing for forward and backward movement of the lower jaw, similar to the streptostyly seen in living squamates, with an estimated force output of 1907 newtons.
• Four types of tessellated pavements are recognized: tessellated pavements formed by jointing; tessellated pavements formed by cooling contraction; tessellations formed by mud cracking and lithification; and tessellated sandstone pavements of uncertain origin.
• Columnar jointing can occur in cooling lava flows and ashflow tuffs (ignimbrites), as well as in some shallow intrusions.
• Surprisingly, it exhibits a form of paracraniokinesis in which the dentary bone articulates against the surangular bone, further jointing the lower jaw and hypothetically allowing this animal a wider array of hunting strategies.
• If a mudfield is repeatedly wetted and dried, it can be annealed to a pattern dominated by Y-shaped junctions, as it is thermodynamically favored like columnar jointing and polygonal patterned ground.
• Similar red lead-based compounds were also widely used as a jointing compound in engineering, to form steam- or oil-tight flanged joints in pipework.
• Mathews based his suggestion on the age of the underlying till, the existence of pillow lava close to the bottom of some lavas that indicate subaqueous volcanism, horizontal jointing at the edges of the lavas that indicate rapid cooling, and the absence of apparent paleotopography to explain these features.
• Mathews based this on the age of the underlying glacial till, the existence of pillow lava close to the bottom of some lavas, indicating subaqueous volcanism, the columnar jointing at the edges of the lavas, indicating rapid cooling, and the absence of apparent palaeogeography.
• Mathews based this on the age of the underlying till, the existence of pillow lava close to the bottom of some lavas, indicating subaqueous volcanism, the columnar jointing at the edges of the lavas, indicating rapid cooling, and the absence of apparent palaeogeography.
• Dhinodhar Hill, is a volcanic plug rising above the local sandstone, and composed of relatively fresh, very fine-grained, black to dark grey, largely aphyric (largely without phenocrysts), aphanitic rock, rising to an elevation of 386 meters, it shows several near- vertical, dike-like tabular intrusions with well-developed columnar jointing, and a roughly circular ring breached to the east, enclosing a pronounced crater-like central depression.

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