A pier chart is used to compare relative parts of a whole.
If an action is repeated n times and a certain event occurred b times then the ratio b/n is called the relative frequency.Where as theoretical probability is used to determine the number of ways that the event can occur if an experiment is repeated a large number of times.
Absolute value uses a companies cash flow to determine it's worth. Relative value compares a companies worth to other competitors.
Means a device which measures the angle of the boom relative to horizontal. Enable to determine measurements to a precision degree.
first derivative = 6x2 + 6x - 36 factors are (6x + 18)(x - 2)
Relative age is used to determine the age and how old a geological feature or fossil.
fossils can be used to determine the relative age of rock layer by using the classification of fossils to find the relative ages of rocks in which fossils are found. :] hoped i helped you out.
The color wheel is typically used to determine the relative color of objects with pigments, where contrasting or complementary colors are often chosen.
Reference points are used to determine motion by comparing the position of an object relative to those points over time. If the object changes its position relative to the reference points, then motion has occurred. By observing the changes in the object's position relative to fixed points, we can determine its motion, speed, and direction.
Job Evaluation is the way it used to
By using the geologic time scale. Certain organisms are only found during certain times and if a fossil of one of these organisms is found then you can determine the relative age of the fossil.
The Mohs scale is used to determine the relative hardness of minerals.
They are used to determine the relative ages of rocks by stating that younger rocks lie above older rocks, and that rocks that cut through a layer are younger than the existing layer.
The guidelines used to determine the relative ages of the rocks and events shown by a geologic cross-section is the Law of Superposition. It is the basic law of geochronology.
Fossils can be used to determine the relative age of rock layers by comparing the types of fossils found in different layers. Fossils of organisms that existed for a short period of time can be used to date layers of rock containing them. Geologic features such as fault lines and unconformities can also help determine the relative age of rock layers by showing where layers have been disturbed or eroded.
The process that places geologic events in proper time sequence is referred to as relative dating. This method involves analyzing the layers of rock or fossils to determine their relative age compared to each other.
Index fossils can be used to help determine the relative age of rock layers. Index fossils are from species that only existed for a short time. Index fossils are found in rock layers. Trilobites and Graptolites are index fossils.