Explanation:

The theory of Isostasy was developed by C.E. Dutton.

Isostasy:

Isostasy is a concept in geology that explains the equilibrium of the Earth's crust. It suggests that the Earth's crust is floating on a denser, more fluid layer called the asthenosphere. The principle of isostasy states that the lithosphere, which includes both the crust and the uppermost part of the mantle, is in a state of equilibrium and adjusts vertically to maintain balance.

Development of the Theory:

The theory of Isostasy was developed by Clarence Edward Dutton, an American geologist and US Army officer. Dutton conducted extensive research on the geology of the western United States and made significant contributions to the understanding of geological processes.

Dutton's work on the theory of Isostasy was published in his book "Report on the Geology of the High Plateaus of Utah" in 1880. In this book, he proposed the concept of isostasy to explain the uplifted mountains and deep valleys in the region.

Key Points:

- Clarence Edward Dutton developed the theory of Isostasy.
- He proposed the concept in his book "Report on the Geology of the High Plateaus of Utah" in 1880.
- The theory explains the equilibrium of the Earth's crust and the vertical adjustment of the lithosphere.
- Isostasy suggests that the Earth's crust floats on a denser, more fluid layer called the asthenosphere.
- Dutton's research on the geology of the western United States contributed significantly to the understanding of geological processes.

Conclusion:

The theory of Isostasy was developed by Clarence Edward Dutton. His research and contributions to the understanding of geological processes, particularly in the western United States, have had a significant impact on the field of geology.