Table of Contents
- 1 What is it called when we compare the age of two rock layers to each other?
- 2 What are 2 rules used to determine ages of rock layers?
- 3 How does correlation explain the relative age of rocks?
- 4 What are the guidelines used to determine the relative ages of the rocks and events shown by a geologic cross section?
- 5 How are rocks of the same age different on different continents?
- 6 Why is a younger rock layer than C?
- 7 Why do metamorphic rocks form at the same time?
What is it called when we compare the age of two rock layers to each other?
The relative age of a rock is its age in comparison with other rocks. If you know the relative ages of two rock layers, you know which is older and which is younger, but you do not know how old the layers are in years.
What are 2 rules used to determine ages of rock layers?
Simply stated, each bed in a sequence of sedimentary rocks (or layered volcanic rocks) is younger than the bed below it and older than the bed above it. This law follows two basic assumptions: (1) the beds were originally deposited near horizontal, and (2) the beds were not overturned after their deposition.
What are the two types of ages of rocks?
There are two main ways to determine the age of a rock, these are Relative dating and Absolute dating. Relative dating is used to determine the relative order of past events by comparing the age of one object to another.
How does correlation explain the relative age of rocks?
—A process by which the age of a rock can be determined by studying the relative concentrations of a radioactive isotope and the products formed by its decay. —The principle that a layer of rocks is older than any other layer that lies above it and younger than any other layer that lies below it.
What are the guidelines used to determine the relative ages of the rocks and events shown by a geologic cross section?
The relative age of a rock is its age compared to the ages of other rocks. First and foremost, they use the law of superposition to determine the relative ages of sedimentary rock layers. According to the law of superposition, in horizontal sedimentary rock layers the oldest is at the bottom.
What do Earth’s rock layers reveal?
The location of fossils in rock layers provides evidence of Earth’s past landscapes. It is hard to guess the age of rock. Scientists have to act like detectives, piecing together a mystery to determine how long ago rocks formed. Fossils found in a particular rock layer help scientists determine the age of the rock.
How are rocks of the same age different on different continents?
Geologists noted that for rocks of the same age but on different continents, the little magnets pointed to different magnetic north poles. For example, 400-million-year-old magnetite in Europe pointed to a different north magnetic pole than the same-aged magnetite in North America.
Why is a younger rock layer than C?
(2) A is younger than C, because the intrusion of A metamorphosed part of rock layer C. (3) A is older than C, because A has older index fossils. (4) A is older than C, because the intrusion of A cuts across rock layer C. Page 9
How is the relative age of the layers determined?
Applying the Law of Superposition to determine the relative ages of the layers, the observer gets the relative ages of the layers reversed. To apply the Law of Superposition successfully, some independent way of recognizing ‘top’ from ‘bottom’ within a sequence is needed.
Why do metamorphic rocks form at the same time?
In metamorphic rocks, layering may develop in response to application of pressure. In that case, the layers may all form at the same time. The position of a layer within the series, above or below another layer, will not be indicative of whether it is younger or older.
https://www.youtube.com/watch?v=Aff8s-FEtv8