by MeganL677 Fri Apr 06, 2018 11:47 pm
I was also stuck btw D and E.
To address answer choice D's scale problem, I think both glacier and earthquake are a very large scale event compared with the growth rate of lichens, so the scale shouldn't be the problem here. I chose it wrong because I didn't understand how the lichen method work.
The pattern is:
Firstly, lichens quickly colonize on newly exposed rocks. That is, to set foot on a "point" of the newly exposed stone within a relevant short time.
Secondly, they expand from the original "point" very slowly on these newly exposed rocks. After a few centuries(e.g 500 years), when those newly exposed rocks become old rocks, they only expand: 5*9.5mm/century=47.5mm in total. That is still a very small corner on a rock, which implies it's nearly impossible for the lichens to connect together from rocks to rocks in several hundred years....
However, if we deny that fact, if some lichens could grow very rapidly on the rocks, too soon they would have expanded to connect together to see when the rock fell...
Along the earthquake line, there are a lot of such rocks with spotted lichens, this is how we can detect the location of the earthquake.
Let's roughly set a formula:
largest lichen diameter/ lichen's constant growth speed= how many years the lichen has settled on the rock (ignore the quickly colonize time)= for how many years the rocks were exposed.
Thus we could know when did the earthquake or glacier receding (whatever event that would expose some new rocks) occurred.
This formula could also explain why the conditions influencing lichen's growth rate can be disturbing- they can't simply divide it when it's not constant and must factor in those conditions in the formula, which would make the formula much more complex.
In a nutshell, it is exactly because of the slow growth rate of lichens, rather than the rapid growth rate, can we determine when and where did those geological events happen.
I don't know if the above understanding is accurate, please note me if I was wrong!