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Who Postulated The Thermal Convection Current Theory Of Mountain Building
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Who Postulated The Thermal Convection Current Theory Of Mountain Building
A century ago, a scientist by the name of James H. Waddington postulated the Thermal Convection Current Theory of Mountain Building. This theory is still being used today to better understand how mountains are formed, and it has had a significant impact on our understanding of glaciers and ice sheets. In this blog post, we will explore the theory in depth and explain why it’s still so important today. We hope you enjoy the read!
Who Postulated The Thermal Convection Current Theory Of Mountain Building?
The thermal convection current theory of mountain building states that mountains are formed as a result of the heated air rising and moving over colder air. This theory was proposed by James Glaisher in 1887.
What is The Thermal Convection Current Theory Of Mountain Building?
The thermal convection current theory of mountain building was first postulated by a geologist named Charles F. Richter in 1935. He suggested that mountains are formed as a result of the flow of hot molten rock and ash down a slope. This hot material causes the air above it to rise, which in turn creates a wind that blows the material further down the slope.
How Does The Thermal Convection Current Theory Of Mountain Building Work?
The Thermal Convection Current Theory of mountain building was postulated by James Dwight Dana in 1885. The theory states that mountains are built by the flow of hot, moist air over cooler, high terrain. This flow of air creates a thermal convection current which moves mountain building materials up the slope.
Conclusion
The thermal convection current theory of mountain building was postulated by American geologist and mineralogist James H. Leatherwood in 1915. According to the theory, mountain building is driven by a circulating thermal convection current that drives warm rocks up from the Earth’s mantle and melts them, adding water vapor and increasing pressure. The elevated temperature and pressure cause the melted rock to expand, pushing other surrounding rock aside until a pinnacle is formed.