isogeotherm Synonyms

No Synonyms and anytonyms found

isogeotherm Meaning

Webster

isogeotherm (n.)

A line or curved surface passing beneath the earth's surface through points having the same mean temperature.

isogeotherm Sentence Examples

  1. Isogeotherms are lines that connect points of equal temperature in the Earth's crust.
  2. The rate of increase in temperature with depth, known as the geothermal gradient, is not constant but varies with location and isogeotherm.
  3. In general, the temperature gradient increases with depth, meaning that the isogeotherms are closer together at greater depths.
  4. Isogeotherms can be used to study the Earth's internal structure and heat flow.
  5. By measuring the temperature gradient in a borehole, geophysicists can determine the depth to the basement rocks and the thickness of the sedimentary layers.
  6. Isogeotherms can also be used to estimate the amount of heat flowing from the Earth's interior to the surface.
  7. This information is important for understanding the Earth's energy budget and for modeling climate change.
  8. The isogeotherm pattern in a region can be affected by a variety of factors, including the presence of groundwater, the topography of the land surface, and the thermal conductivity of the rocks.
  9. Isogeotherms can also be used to locate geothermal reservoirs, which are areas of the Earth's crust where the temperature is high enough to generate electricity.
  10. Geothermal reservoirs are typically found in areas of high heat flow, such as near volcanoes or along plate boundaries.

FAQs About the word isogeotherm

A line or curved surface passing beneath the earth's surface through points having the same mean temperature.

No synonyms found.

No antonyms found.

Isogeotherms are lines that connect points of equal temperature in the Earth's crust.

The rate of increase in temperature with depth, known as the geothermal gradient, is not constant but varies with location and isogeotherm.

In general, the temperature gradient increases with depth, meaning that the isogeotherms are closer together at greater depths.

Isogeotherms can be used to study the Earth's internal structure and heat flow.