Strange, but I didn't get that message from Bob that you responded to- but 
coincidentally I sent the following to Bob earlier:

***
  It's often said that in areas where the bedrock is very mixed doesn't 
correlate all that strongly with the vegetation in glaciated areas because the 
soil was pushed around (till) and all mixed up but there still has to be some 
correlation. At least it's a factor along with the protection MTSF gets from 
having high hills nearby. The high hills not only offer protection but lots of 
water draining down from on high- and nutrients draining down with that water. 
Probably the biggest factor of all though is the fact that those stands were 
not cut- similar good terrain is probably common and should have had similar 
great trees.

  I think the lesson learned is that PROTECTION is the most important thing- 
which is why we must continue to protect other forests that have the potential 
to also be great, even if it's centuries from now.

  Wild guess but I suspect there must be many similar pockets of trees in the 
NE that were not cut - which simply haven't been discovered by big tree lovers.
***

To give some background on the volcanic origin of the bedrock of MTSF: first we 
need to realize that central Mass- a hour's drive east of MTSF is the boundary 
between the ancient continents of Laurasia and Gondwanaland- just a few miles 
east of my house. The area just west of the Connecticut Valley (which didn't 
exist that far back) was a chain of volcanic islands. The erosion of those 
islands and deposition as sedimentary rocks is the origin of several rock 
formations extending from Greenfield westerly to just west of MTSF. Those rock 
formations were later compressed and faulted.
Joe
  ----- Original Message ----- 
  From: Edward Frank 
  To: [email protected] 
  Sent: Wednesday, August 12, 2009 11:39 PM
  Subject: [ENTS] Geology of Todd and Clark Mountains, MTSF, MA


  Bob,

  You have hinted several times for me to look at the geology of MTSF.  Here is 
a basic summary of what I found.  There is much more data I looked at, but much 
of it is pretty esoteric.  Attached is a geologic map of the Mohawk Trails Area 
- Todd  Mountain



  Moretown Formation   Om   
http://tin.er.usgs.gov/geology/state/sgmc-unit.php?unit=MAOm;0  This correlates 
with the Beauceville Formation:  The Beauceville Formation of the Magog Group 
is mainly composed of graptolitebearing pelagic mudstone and volcaniclastic 
rocks, which were deposited in a fore-arc basin during the Ordovician. The 
volcaniclastic rocks of the Beauceville area, their transport and depositional 
mechanisms are not well known.  
http://theses.uqac.ca/resume_these.php?idnotice=10982977&lang=en   Simlarly it 
is correlated with the Missisquoi Formation of VT  which is described as a 
metasedimentary sequence that has undergone multiple episodes of deformation.  

  Gneiss at Hallockville Pond    Ohpg  
http://tin.er.usgs.gov/geology/state/sgmc-unit.php?unit=MAOhpg;0

  Hawley Formation   Oh  
http://tin.er.usgs.gov/geology/state/sgmc-unit.php?unit=MAOh;0

  Geologic Map  http://mrdata.usgs.gov/sgmc/ma.html

  The rocks on Clark and Todd Mountains are metasedimentary rocks that have 
undergone several episodes of deformation,  The original rocks that formed the 
sediment may have been of volcanic origin, but it was eroded, transported, and 
deposited as sediment before it lithified into the original bedock before 
deformation.  There is a possibility of some igneous intrusions into the 
metasedimentary rocks, but none are mapped ion the area of Clark or Todd 
Mountians

  Ed




  "The most beautiful thing we can experience is the mysterious. 
  It is the source of all true art and all science." - Albert Einstein
    ----- Original Message ----- 
    From: Bob 
    To: ENTS 
    Sent: Wednesday, August 12, 2009 10:12 PM
    Subject: [ENTS] Sun, Mike, Joe, and Me



         ENTS

            Today the above named hiked in MTSF. We'll likely all post  
    pictures, but just a few observations sent from my trusty iPhone.
             Joe examined rocks on Todd and Clark Mtns and observed  
    complex geology. Heavily metamorphized rocks that I loosely called  
    schist appear to have a volcanic origin. I'll let Joe address the  
    subject, but if Joe is correct and I suspect he is, then the mineral  
    content of the rocks is probably very rich.

    Mike,

         Would you mind sharing your thoughts on what you saw today?

    Bob


    Sent from my iPhone
    

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