Thyssen gravity meter with accessories

A gravity meter, or gravimeter, is an instrument designed to measure and record variations in the earth’s gravitational field in specific locations. These instruments can be broadly divided into two types, stable/static and unstable/astatic. The key difference is that a stable gravity meter will reset itself once it has made a measurement of gravity, whilst an unstable gravity meter will not reset or return to a neutral position.

The benefit of unstable meters is that they exaggerate the changes in gravity making them easier to measure with high precision. The downside to unstable meters is that they are, by design, very sensitive to other factors such as additional sources of gravity, movement, and even heat.

This Thyssen gravity meter is a relatively early design of unstable gravity meter, which uses a quartz beam placed on a knife-edge with a 20-gram platinum balance weight placed on the end of one arm, and spring balance one the other. A small 1-gram balance is placed on a slider, and as the operator slides the smaller balance along the beam, and the platinum weight on the other end of the beam will move based on the strength of the specific gravity of the area being recorded.

These measurements (called deflections) are often very slight and need to be observed via a microscope and can also be used to extrapolate the density and structure of the earth’s crust. This made gravity meter such as this one very useful as a means of prospecting for mineral, oil and ore deposits. Thyssen gravity meters are especially sensitive to changes in temperature which would affect the spring balance, and therefore the instrument also has a thermometer in a lagged tube.

A gravity meter, or gravimeter, is an instrument designed to measure and record variations in the earth’s gravitational field in specific locations. These instruments can be broadly divided into two types, stable/static and unstable/astatic. The key difference is that a stable gravity meter will reset itself once it has made a measurement of gravity, whilst an unstable gravity meter will not reset or return to a neutral position.

The benefit of unstable meters is that they exaggerate the changes in gravity making them easier to measure with high precision. The downside to unstable meters is that they are, by design, very sensitive to other factors such as additional sources of gravity, movement, and even heat.

This Thyssen gravity meter is a relatively early design of unstable gravity meter, which uses a quartz beam placed on a knife-edge with a 20-gram platinum balance weight placed on the end of one arm, and spring balance one the other. A small 1-gram balance is placed on a slider, and as the operator slides the smaller balance along the beam, and the platinum weight on the other end of the beam will move based on the strength of the specific gravity of the area being recorded.

These measurements (called deflections) are often very slight and need to be observed via a microscope and can also be used to extrapolate the density and structure of the earth’s crust. This made gravity meter such as this one very useful as a means of prospecting for mineral, oil and ore deposits. Thyssen gravity meters are especially sensitive to changes in temperature which would affect the spring balance, and therefore the instrument also has a thermometer in a lagged tube.

A gravity meter, or gravimeter, is an instrument designed to measure and record variations in the earth’s gravitational field in specific locations. These instruments can be broadly divided into two types, stable/static and unstable/astatic. The key difference is that a stable gravity meter will reset itself once it has made a measurement of gravity, whilst an unstable gravity meter will not reset or return to a neutral position.

The benefit of unstable meters is that they exaggerate the changes in gravity making them easier to measure with high precision. The downside to unstable meters is that they are, by design, very sensitive to other factors such as additional sources of gravity, movement, and even heat.

This Thyssen gravity meter is a relatively early design of unstable gravity meter, which uses a quartz beam placed on a knife-edge with a 20-gram platinum balance weight placed on the end of one arm, and spring balance one the other. A small 1-gram balance is placed on a slider, and as the operator slides the smaller balance along the beam, and the platinum weight on the other end of the beam will move based on the strength of the specific gravity of the area being recorded.

These measurements (called deflections) are often very slight and need to be observed via a microscope and can also be used to extrapolate the density and structure of the earth’s crust. This made gravity meter such as this one very useful as a means of prospecting for mineral, oil and ore deposits. Thyssen gravity meters are especially sensitive to changes in temperature which would affect the spring balance, and therefore the instrument also has a thermometer in a lagged tube.

A gravity meter, or gravimeter, is an instrument designed to measure and record variations in the earth’s gravitational field in specific locations. These instruments can be broadly divided into two types, stable/static and unstable/astatic. The key difference is that a stable gravity meter will reset itself once it has made a measurement of gravity, whilst an unstable gravity meter will not reset or return to a neutral position.

The benefit of unstable meters is that they exaggerate the changes in gravity making them easier to measure with high precision. The downside to unstable meters is that they are, by design, very sensitive to other factors such as additional sources of gravity, movement, and even heat.

This Thyssen gravity meter is a relatively early design of unstable gravity meter, which uses a quartz beam placed on a knife-edge with a 20-gram platinum balance weight placed on the end of one arm, and spring balance one the other. A small 1-gram balance is placed on a slider, and as the operator slides the smaller balance along the beam, and the platinum weight on the other end of the beam will move based on the strength of the specific gravity of the area being recorded.

These measurements (called deflections) are often very slight and need to be observed via a microscope and can also be used to extrapolate the density and structure of the earth’s crust. This made gravity meter such as this one very useful as a means of prospecting for mineral, oil and ore deposits. Thyssen gravity meters are especially sensitive to changes in temperature which would affect the spring balance, and therefore the instrument also has a thermometer in a lagged tube.

A gravity meter, or gravimeter, is an instrument designed to measure and record variations in the earth’s gravitational field in specific locations. These instruments can be broadly divided into two types, stable/static and unstable/astatic. The key difference is that a stable gravity meter will reset itself once it has made a measurement of gravity, whilst an unstable gravity meter will not reset or return to a neutral position.

The benefit of unstable meters is that they exaggerate the changes in gravity making them easier to measure with high precision. The downside to unstable meters is that they are, by design, very sensitive to other factors such as additional sources of gravity, movement, and even heat.

This Thyssen gravity meter is a relatively early design of unstable gravity meter, which uses a quartz beam placed on a knife-edge with a 20-gram platinum balance weight placed on the end of one arm, and spring balance one the other. A small 1-gram balance is placed on a slider, and as the operator slides the smaller balance along the beam, and the platinum weight on the other end of the beam will move based on the strength of the specific gravity of the area being recorded.

These measurements (called deflections) are often very slight and need to be observed via a microscope and can also be used to extrapolate the density and structure of the earth’s crust. This made gravity meter such as this one very useful as a means of prospecting for mineral, oil and ore deposits. Thyssen gravity meters are especially sensitive to changes in temperature which would affect the spring balance, and therefore the instrument also has a thermometer in a lagged tube.

A gravity meter, or gravimeter, is an instrument designed to measure and record variations in the earth’s gravitational field in specific locations. These instruments can be broadly divided into two types, stable/static and unstable/astatic. The key difference is that a stable gravity meter will reset itself once it has made a measurement of gravity, whilst an unstable gravity meter will not reset or return to a neutral position.

The benefit of unstable meters is that they exaggerate the changes in gravity making them easier to measure with high precision. The downside to unstable meters is that they are, by design, very sensitive to other factors such as additional sources of gravity, movement, and even heat.

This Thyssen gravity meter is a relatively early design of unstable gravity meter, which uses a quartz beam placed on a knife-edge with a 20-gram platinum balance weight placed on the end of one arm, and spring balance one the other. A small 1-gram balance is placed on a slider, and as the operator slides the smaller balance along the beam, and the platinum weight on the other end of the beam will move based on the strength of the specific gravity of the area being recorded.

These measurements (called deflections) are often very slight and need to be observed via a microscope and can also be used to extrapolate the density and structure of the earth’s crust. This made gravity meter such as this one very useful as a means of prospecting for mineral, oil and ore deposits. Thyssen gravity meters are especially sensitive to changes in temperature which would affect the spring balance, and therefore the instrument also has a thermometer in a lagged tube.

A gravity meter, or gravimeter, is an instrument designed to measure and record variations in the earth’s gravitational field in specific locations. These instruments can be broadly divided into two types, stable/static and unstable/astatic. The key difference is that a stable gravity meter will reset itself once it has made a measurement of gravity, whilst an unstable gravity meter will not reset or return to a neutral position.

The benefit of unstable meters is that they exaggerate the changes in gravity making them easier to measure with high precision. The downside to unstable meters is that they are, by design, very sensitive to other factors such as additional sources of gravity, movement, and even heat.

This Thyssen gravity meter is a relatively early design of unstable gravity meter, which uses a quartz beam placed on a knife-edge with a 20-gram platinum balance weight placed on the end of one arm, and spring balance one the other. A small 1-gram balance is placed on a slider, and as the operator slides the smaller balance along the beam, and the platinum weight on the other end of the beam will move based on the strength of the specific gravity of the area being recorded.

These measurements (called deflections) are often very slight and need to be observed via a microscope and can also be used to extrapolate the density and structure of the earth’s crust. This made gravity meter such as this one very useful as a means of prospecting for mineral, oil and ore deposits. Thyssen gravity meters are especially sensitive to changes in temperature which would affect the spring balance, and therefore the instrument also has a thermometer in a lagged tube.

A gravity meter, or gravimeter, is an instrument designed to measure and record variations in the earth’s gravitational field in specific locations. These instruments can be broadly divided into two types, stable/static and unstable/astatic. The key difference is that a stable gravity meter will reset itself once it has made a measurement of gravity, whilst an unstable gravity meter will not reset or return to a neutral position.

The benefit of unstable meters is that they exaggerate the changes in gravity making them easier to measure with high precision. The downside to unstable meters is that they are, by design, very sensitive to other factors such as additional sources of gravity, movement, and even heat.

This Thyssen gravity meter is a relatively early design of unstable gravity meter, which uses a quartz beam placed on a knife-edge with a 20-gram platinum balance weight placed on the end of one arm, and spring balance one the other. A small 1-gram balance is placed on a slider, and as the operator slides the smaller balance along the beam, and the platinum weight on the other end of the beam will move based on the strength of the specific gravity of the area being recorded.

These measurements (called deflections) are often very slight and need to be observed via a microscope and can also be used to extrapolate the density and structure of the earth’s crust. This made gravity meter such as this one very useful as a means of prospecting for mineral, oil and ore deposits. Thyssen gravity meters are especially sensitive to changes in temperature which would affect the spring balance, and therefore the instrument also has a thermometer in a lagged tube.

A gravity meter, or gravimeter, is an instrument designed to measure and record variations in the earth’s gravitational field in specific locations. These instruments can be broadly divided into two types, stable/static and unstable/astatic. The key difference is that a stable gravity meter will reset itself once it has made a measurement of gravity, whilst an unstable gravity meter will not reset or return to a neutral position.

The benefit of unstable meters is that they exaggerate the changes in gravity making them easier to measure with high precision. The downside to unstable meters is that they are, by design, very sensitive to other factors such as additional sources of gravity, movement, and even heat.

This Thyssen gravity meter is a relatively early design of unstable gravity meter, which uses a quartz beam placed on a knife-edge with a 20-gram platinum balance weight placed on the end of one arm, and spring balance one the other. A small 1-gram balance is placed on a slider, and as the operator slides the smaller balance along the beam, and the platinum weight on the other end of the beam will move based on the strength of the specific gravity of the area being recorded.

These measurements (called deflections) are often very slight and need to be observed via a microscope and can also be used to extrapolate the density and structure of the earth’s crust. This made gravity meter such as this one very useful as a means of prospecting for mineral, oil and ore deposits. Thyssen gravity meters are especially sensitive to changes in temperature which would affect the spring balance, and therefore the instrument also has a thermometer in a lagged tube.