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CROSSWORD
ANSWER

confining

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The answer CONFINING has 4 possible clue(s) in existing crosswords.

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The word CONFINING is VALID in some board games. Check CONFINING in word games in Scrabble, Words With Friends, see scores, anagrams etc.

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Definitions of confining in various dictionaries:

verb - place limits on (extent or access)

verb - restrict or confine, "I limit you to two visits to the pub a day"

verb - prevent from leaving or from being removed

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Keep reading for additional results and analysis below.

Possible Crossword Clues
Imprisonment is making a criminal pay
Imprisoning
Jailing fascists caught in specious activity?

Last Seen in these Crosswords & Puzzles
Dec 1 2012 The Times - Cryptic
Aug 8 2009 The Telegraph - Quick
Mar 28 2002 The Guardian - Cryptic crossword
Mar 28 2002 The Guardian - Cryptic crossword

Possible Dictionary Clues
Present participle of confine.
keep or restrict someone or something within certain limits of (space, scope, or time).
Keep or restrict someone or something within certain limits of (space, scope, or time)
The borders or boundaries of a place, especially with regard to their restricting freedom of movement.
restricting the scope or freedom of action
crowded

Confining might refer to
Overburden pressure, also called lithostatic pressure, confining pressure or vertical stress, is the pressure or stress imposed on a layer of soil or rock by the weight of overlying material. * The Oxford Dictionary of Earth Sciences describes 'confining pressure' as "the combined hydrostatic stress and lithostatic stress; i.e. the total weight of the interstitial pore water and rock above a specified depth." * Confining pressure might influence ductile behavior of rocks as well. Ductile behavior is enhanced where high * confining pressures are combined with high temperatures and low rates of strain, conditions characteristic of deeper crustal levels.The overburden pressure at a depth z is given by* * * * p * ( * z * ) * = * * p * * 0 * * * + * g * * ∫ * * 0 * * * z * * * ρ * ( * z * ) * * d * z * * * {\displaystyle p(z)=p_{0}+g\int _{0}^{z}\rho (z)\,dz} * where ρ(z) is the density of the overlying rock at depth z and g is the acceleration due to gravity. p0 is the datum pressure, the pressure at the surface. * In deriving the above equation it is assumed that gravitational acceleration g is a constant over z, since it is placed outside the integral. In reality, g is a (non-constant) function of z and should appear inside the integral. But since g varies little over depths which are a very small fraction of the Earth's radius, it is placed outside the integral in practice for most near-surface applications which require an assessment of lithostatic pressure. In deep-earth geophysics/geodynamics, gravitational acceleration varies significantly over depth and g may not be assumed to be constant. * This should be compared with the equivalent concept of hydrostatic pressure in hydrodynamics.

Confining might refer to

Overburden pressure, also called lithostatic pressure, confining pressure or vertical stress, is the pressure or stress imposed on a layer of soil or rock by the weight of overlying material.
* The Oxford Dictionary of Earth Sciences describes 'confining pressure' as "the combined hydrostatic stress and lithostatic stress; i.e. the total weight of the interstitial pore water and rock above a specified depth."
* Confining pressure might influence ductile behavior of rocks as well. Ductile behavior is enhanced where high
* confining pressures are combined with high temperatures and low rates of strain, conditions characteristic of deeper crustal levels.The overburden pressure at a depth z is given by*
*
*
* p
* (
* z
* )
* =
*
* p
*
* 0
*
*
* +
* g
*
* ∫
*
* 0
*
*
* z
*
*
* ρ
* (
* z
* )
*
* d
* z
*
*
* {\displaystyle p(z)=p_{0}+g\int _{0}^{z}\rho (z)\,dz}
* where ρ(z) is the density of the overlying rock at depth z and g is the acceleration due to gravity. p0 is the datum pressure, the pressure at the surface.
* In deriving the above equation it is assumed that gravitational acceleration g is a constant over z, since it is placed outside the integral. In reality, g is a (non-constant) function of z and should appear inside the integral. But since g varies little over depths which are a very small fraction of the Earth's radius, it is placed outside the integral in practice for most near-surface applications which require an assessment of lithostatic pressure. In deep-earth geophysics/geodynamics, gravitational acceleration varies significantly over depth and g may not be assumed to be constant.
* This should be compared with the equivalent concept of hydrostatic pressure in hydrodynamics.

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