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Rate of Geothermal Temperature
| LaTeX Math Inline |
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| body | --uriencoded--T_G(%7B\bf r%7D) |
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change along True Vertical Direction with no account of effects of the seasonal/daily temperature variations ( which are only noticeable above Neutral Temperature Layer ):
Ratio of true vertical component of regional Earth's Heat Flux
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| body | --uriencoded--j_z(%7B\bf r%7D) |
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to the subsurface
Thermal Conductivity | LaTeX Math Inline |
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| body | --uriencoded--\lambda_e(%7B\bf r%7D) |
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at a certain
subsurface point | LaTeX Math Inline |
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| body | --uriencoded--%7B\bf r%7D |
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:
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The most common value of Unbiased Geothermal Temperature Gradient away (GT) away from tectonic plate boundaries boundaries : GT 030 °C.
See Also
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Geology / Geothermal Temperature Field
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