According to the law of crosscutting relationships, any geological feature that cuts across another must be younger than the feature it disrupts. In this case, if a fault ends at an unconformity, it indicates that the fault must be older than the unconformity because the unconformity represents a period of erosion or non-deposition that occurred after the faulting. Thus, the relative ages can be determined, with the fault being older than the unconformity and the rock layers below the unconformity being older than the fault itself.
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The relationship of a stepbrother's son to someone would be that of a step-nephew. This is because the stepbrother is not biologically related to the person, but is a relative through marriage. Therefore, the stepbrother's son would be the person's step-nephew, as they are the child of the stepbrother.
The half-life of Carbon 14 and radionuclides are used to estimate the absolute (versus relative) age of pre-history items.
Yes, your husband is considered to be your closest relative.
A relative is someone who shares a common ancestor with you. A relative by marriage is someone who does not share an ancestor with you but has married someone who does. In the most common instances of this relationship, the words "in Law" are added to the description of the relative. For example, a Brother in law is someone who is married to your sister, or is the brother of your wife. The word being looked for is "Affine" Kinsman or Kinswoman
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.
No, the law of crosscutting relationships can apply to any type of rock. It states that a geological feature must be younger than the rock it cuts across. This principle helps geologists determine the relative ages of rocks and geological events.
The relative age of a fault or igneous intrusion that cuts through an unconformity is younger than the unconformity but older than the rock it cuts through. This is because the fault or intrusion must have formed after the deposition of the rock layers below the unconformity but before the deposition of the rock layers above the unconformity.
If a fault or intrusion cuts through an unconformity, the fault or intrusion is younger than all the rocks it cuts through above and below the unconformity.
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.
Relatively, they are younger than the rock they cut through.
To determine relative humidity using temperature as a reference point, you can use a psychrometric chart or an online calculator. By knowing the temperature and the dew point, you can calculate the relative humidity. The relationship between temperature and relative humidity is important in understanding the moisture content in the air.
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Relative age is determined by the principle of superposition in geology, which states that in any undisturbed sequence of rock layers, the youngest layer is at the top and the oldest layer is at the bottom. By observing the order of rock layers, geologists can determine which layer is older or younger relative to others based on their position.
The circle of fifths helps musicians determine the relative minor key of a musical composition by showing the relationship between major and minor keys. The key that is a minor third below a major key on the circle of fifths is its relative minor key.
Relative age is used to determine the age and how old a geological feature or fossil.
To determine the relative minor of a major key, you can find the sixth note of the major scale. This note is the starting point for the relative minor scale.