Skip to content
Theory of Isostasy
-
What did Joly think about the density above and below the level of compensation?
Options:
- Density remains uniform both above and below the level of compensation
- Density varies both above and below the level of compensation
- Density varies above the level of compensation but remains uniform below it
- Density varies below the level of compensation but remains uniform above it
-
What did Joly believe about the level of compensation in comparison to the concept of Hayford and Bowie?
Options:
- Joly believed that the level of compensation is a linear phenomenon while Hayford and Bowie believed it is a zonal phenomenon
- Joly believed that the level of compensation is a zonal phenomenon while Hayford and Bowie believed it is a linear phenomenon
- Joly and Hayford and Bowie had the same concept of the level of compensation
- Joly and Hayford and Bowie had contradictory views on the level of compensation
-
According to Arthur Holmes, why do higher columns of the earth’s crust stand?
Options:
- Because they are made of heavier materials
- Because they are supported by lighter material below them for greater depth
- Because they have a smaller surface area
- Because they are not subject to geological events
-
What is the depth at which isostatic compensation occurs in areas that have not been disturbed by geological events for a longer duration?
Options:
- 25 km
- 50 km
- 75 km
- 100 km
-
How did Holmes and L. Holmes attempt to illustrate the concept of equal weight along the ‘level of equal pressure’?
Options:
- Through a diagram of four columns of equal cross-section
- Through a diagram of the earth's magnetic field
- Through a diagram of the earth's tectonic plates
- Through a diagram of the earth's mantle
-
How did Holmes and L. Holmes determine the weight of each column along the level of equal pressure?
Options:
- By measuring the surface area of each column
- By multiplying the density and corresponding thickness down to the depth of 50 km
- By measuring the pressure on the underlying mantle
- By calculating the total weight of each column
-
How did Holmes and L. Holmes explain the concept of isostasy?
Options:
- Through a diagram of the earth's tectonic plates
- Through a diagram of the earth's mantle
- Through a diagram of the earth's magnetic field
- Through a diagram of characteristic examples of crustal columns with the same area and extending downward to the same depth below sea-level
-
Why is there no complete isostatic adjustment over the globe?
Options:
- Due to sudden climatic changes at an extensive global scale
- Because of geological forces coming from within the earth
- Due to disagreement among the scientists about the nature of isostasy
- All of the above
-
What happens when a newly formed mountain undergoes severe denudation?
Options:
- The mountainous area becomes heavier and the oceanic floor becomes lighter
- The oceanic floor becomes heavier and the mountainous area becomes lighter
- The state of balance or isostasy between the two areas is not disturbed
- None of the above
-
What is the cause of disturbances in the ideal condition of isostasy?
Options:
- Exogenetic forces
- Climatic changes
- Endogenetic forces
- Sedimentation
-
How is isostatic balance maintained between mountainous areas and oceanic floors?
Options:
- Through the removal of sediments from the oceanic floor
- Through the flowage of heavier materials from the substratum towards the rising column of the mountain
- Through the deposition of sediments on the oceanic floor
- Through the removal of materials from the mountainous area
-
What happens when endogenetic forces act suddenly and violently?
Options:
- The state of isostatic balance is maintained
- The process of isostatic adjustment through the flowage of materials from the substratum is not maintained
- The mountainous area becomes heavier
- The oceanic floor becomes lighter
-
What caused the subsidence of extensive parts of North America and Eurasia during Pleistocene glaciation?
Options:
- Release of pressure of superincumbent thick load of ice sheets
- Accumulation of thick ice sheets on the land surface
- Climatic changes at a global scale
- Endogenetic forces
-
What is the current rate of isostatic recovery in Scandinavia and Finland?
Options:
- One feet per year
- One feet per 28 years
- 900 feet per year
- 900 feet per 28 years