It is easier to correlate diagrams because all units are scaled down, making it easier to see the "whole picture". In the field, the geologists have to deal with huge tracts of land, which makes it difficult to reconstruct a sequence of events.
It is easier because in the field someone might not be able to see everything clearly and mapped out because of blockage such as vegetation and other things
Relative Dating
If the DNA sequence is ACT, the complimentary mRNA sequence would be UGA
No DNA sequence wont have U (uracil), so it is an RNA sequence!
A small neucleotide sequence is CGGGTACGAAT its complimentry sequence is GCCCATGCTTA
The sequence of the RNA would be UCG-AUG-UGA.
It is easier because in the field someone might not be able to see everything clearly and mapped out because of blockage such as vegetation and other things
Check outhttps://github.com/bramp/js-sequence-diagrams
The main difference between communication diagrams and sequence diagrams is that sequence diagrams are good at showing sequential logic but not that good at giving you a "big picture view" whereas communication diagrams are the exact opposite
Someone looking for a sequence diagram online can find them at various websites. Microsoft is a website which has sequence diagrams. There are many other websites dedicated to sequence diagrams.
Plz tell me the answer
Plz tell me the answer
There are no. of diagrams in computer science .One of these diagrams is the sequence diagram. Sequence are used to represent a software system by a series of events or transaction in the system
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Relative Dating
Within a small area, you can correlate the rocks of one locality with those of another by simply walking along the outcropping edges. However, this might not be possible when the rocks are covered by soil and vegetation. This problem can be corrected if you note the position of a distinctive rock layer in a sequence of strata. You may be able to identify a rock layer in another location if it's composed of very distinctive or uncommon minerals.
They are an observable sequence of rock that exists in the oceanic crust from the surface to the mantle.
At least two states are the minimum.