Definition of isogeotherm in English:

isogeotherm

noun ˌʌɪsə(ʊ)ˈdʒiːə(ʊ)θəːmˌīsəˈjēəTHərm

Geography

A line or surface on a diagram connecting points representing those in the interior of the earth having the same temperature.
〔地理〕等地温线，地下等温线
Example sentencesExamples
- It is a well-known fact that the presence of water in the pores of a rock increases its capacity to conduct heat, so that we may surmise a rise in the local isogeotherm in such situations.

Derivatives

isogeothermal

adjectiveˌʌɪsə(ʊ)dʒiːə(ʊ)ˈθəːm(ə)l

Geography

Origin

Mid 19th century: from iso- 'equal' + geo- 'earth' + Greek thermē 'heat'.

Definition of isogeotherm in US English:

isogeotherm

nounˌīsəˈjēəTHərm

Geography

A line or surface on a diagram connecting points representing those in the interior of the earth having the same temperature.
〔地理〕等地温线，地下等温线
Example sentencesExamples
- It is a well-known fact that the presence of water in the pores of a rock increases its capacity to conduct heat, so that we may surmise a rise in the local isogeotherm in such situations.

Origin

Mid 19th century: from iso- ‘equal’ + geo- ‘earth’ + Greek thermē ‘heat’.

词汇	isogeotherm
释义	Definition of isogeotherm in English: isogeotherm noun ˌʌɪsə(ʊ)ˈdʒiːə(ʊ)θəːmˌīsəˈjēəTHərm Geography A line or surface on a diagram connecting points representing those in the interior of the earth having the same temperature. 〔地理〕等地温线，地下等温线 Example sentencesExamples It is a well-known fact that the presence of water in the pores of a rock increases its capacity to conduct heat, so that we may surmise a rise in the local isogeotherm in such situations. Derivatives isogeothermal adjectiveˌʌɪsə(ʊ)dʒiːə(ʊ)ˈθəːm(ə)l Geography Origin Mid 19th century: from iso- 'equal' + geo- 'earth' + Greek thermē 'heat'. Definition of isogeotherm in US English: isogeotherm nounˌīsəˈjēəTHərm Geography A line or surface on a diagram connecting points representing those in the interior of the earth having the same temperature. 〔地理〕等地温线，地下等温线 Example sentencesExamples It is a well-known fact that the presence of water in the pores of a rock increases its capacity to conduct heat, so that we may surmise a rise in the local isogeotherm in such situations. Origin Mid 19th century: from iso- ‘equal’ + geo- ‘earth’ + Greek thermē ‘heat’.
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