Scientists use the relative amount of stable and unstable isotopes in an object to determine its age.
Carbon-14 dating relies on the fact that due to incidence of cosmic rays on the earth's atmosphere, carbon-14 is constantly being made by reaction with nitrogen in the atmosphere. Now carbon-14 has a half life of about 5500 years, so an equilibrium level of carbon-14 is set up, and over a long period of time remains roughly constant. All living things absorb carbon from the atmosphere in carbon dioxide, but when they die this stops. Therefore at the time of death the ratio of carbon-14 to the stable varieties of carbon has a certain value which is basically considered to have been constant up to today, but after death the carbon-14 starts to decay with the above half life, so if the sample of the dead organic matter is analysed, the present ratio of carbon-14 to stable carbon gives an indication of how long the organic matter has been dead.
In actual practice the process is much more complicated and all sorts of corrections and calibrations have to be made, but that is the principle behind it.
Isotopes are in almost everything in very small amounts. Most isotopes are unstable so will release radiation because they break down into simpler elements to gain stability. By measuring the half-life of these isotopes and by comparing present amounts of the isotopes and the original amounts, they're able to determine the age.
In order for this to work, you need a reference. As an example, the best reference for radioactive dating is carbon dating, which measures the ratio of carbon-14 to carbon-12 and carbon-11 in a sample. This takes advantage of the fact that the carbon-14 ratio is relatively known by comparison with other dating techniques, and on the fact that the carbon-14 ratio is stable until the plant material containing it "dies". The "complexity" in this method is that the carbon-14 ratio was not constant - it varied over time - so compensation techniques are used.
the object your holding is an object.
Usually scientists do not use any tool to determine how strong a tornado is. Usually the strength of a tornado is determined based on the severity of damage it causes. Occasionally wind speed measurements are obtained using Doppler radar, but such measurements are rare.
The average speed of an object can be used to determine an unmeasured distance by using the formula distance = speed x time. The time should also be known for this formula to work.
The answer would be different
Yes it does make it easier by using a fulcrum Yes it does make it easier by using a fulcrum
Archeologists determine how old an object is, by using Carbon Dating.
Scientists can determine the age of some ancient artifacts using carbon-14 dating.
They determine it by using sonar.
relative dating
relative dating
Carbon decay or carbon dating
Scientists can determine the age of some ancient artifacts using Carbon-14 Dating.
Geologists determine the absolute age of rocks using radiometric dating techniques, such as carbon dating or uranium-lead dating. These methods rely on measuring the proportions of radioactive isotopes and their decay products in the rocks to calculate how long ago they formed.
Carbon dating
using sonar waves
Fossil record
The basic requirement for you to see an object using the microscope is light. The amount of light will determine the visibility of the specimen.