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The Geology of Worcester, Massachusetts

The Geology of Worcester, Massachusetts


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This historic book may have numerous typos, missing text or index. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. 1903. Not illustrated. Excerpt: ... is found underlying the central part of Worcester, and which has already been considered, we find in the western part of the city the Carboniferous micaceous quartzite, identical with that found east, and in the midst, of the Carboniferous phyllite. This arrangement of these two formations is due to folding and subsequent erosion, by which the lower one is revealed alongside of the upper. Paxton On following this micaceous quartzite in the ex schist in treme western part of Worcester the rock becomes the plateau. coarser i n grain and abounds in parallelly injected granite, giving an appearance that frequently simulates a metamorphic conglomerate. This western and more highly metamorphosed phase of the Carboniferous quartzite has been called the Paxton schist,1 from its occurrence in that town, just as the similar gneissoid extension of the same quartzite on the east is called the Bolton gneiss. The Paxton schist is less gneissoid than the Bolton gneiss because of a smaller proportion of injected granite. Brimneid Lying above the Paxton schist, as is shown by schist in the its upper position in an anticline in the northwestern plateau. of Worcester, is a rusty, graphitic, fibrolitic mica schist8 identical with the rusty, graphitic, fibrolitic mica schist found in patches within the area of the Bolton gneiss. This rusty schist has been crumpled into almost innumerable folds, both large and small, and contains much injected granite. Lying as it does above the Paxton schist, which is a more highly metamorphosed phase of the Carboniferous quartzite, this rusty schist bears the same relation to the Paxton schist that the Worcester phyllite bears to the Carboniferous quartzite; also on the east side of Worcester there is, in a small area, a transition from the phyllit...


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Product Details
  • ISBN-13: 9781150605895
  • Publisher: General Books
  • Publisher Imprint: General Books
  • Height: 246 mm
  • No of Pages: 66
  • Spine Width: 4 mm
  • Width: 189 mm
  • ISBN-10: 1150605898
  • Publisher Date: 01 Jan 2012
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 136 gr

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