Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meaningsLoomis, Frederic Brewster
Science
Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meanings
Loomis, Frederic Brewster
Minerals -- United States; Rocks -- United States
In order to make a collection valuable two or three rules must be
observed. In the case of rocks, collect large enough samples so that
they will be characteristic, and clear in their make-up. The standard
size for rocks is 3 × 4 inches on top and one to two inches thick
according to the nature of the rock. Tiny fragments do not give the
character of the rock as well, and they are all the time getting into
confusion. Every specimen should be labeled, with at least its name and
the exact locality from which it came. Composition, structural features,
associations, and classification may be added, the more the better; for
each item adds to the information and interest of the specimen. One may
make his own labels or have printed blanks, and may put as much care and
art into the labels as desired, the more the better. One thing is very
important and that is to have a number on the label with a corresponding
one on the specimen, so that in case they should get separated, they may
be readily brought together, even by one who is not familiar with the
individual specimens. Lastly, give your collection as good a place as
possible, either in drawers, boxes or in a case. The specimens are worth
being kept in order and where they can be readily seen and compared.
Nature is systematic, and there is a reason for the order in which rocks
and minerals are taken up. It is desirable either that this order, or
some one of the orders of Nature appear in the collection. In this book
the metals are the basis of classification, all those minerals primarily
related to one of the metals being grouped together.
In collecting minerals, the size of the specimens can not be so
regularly followed, but it should be followed when collecting
non-crystalline minerals, and when possible. Crystals however are chosen
from a variety of points of view, as perfection of form, color, examples
of cleavage, twinning, etc.; so that in many cases smaller or larger
examples must appear in the collection. It is always desirable that as
many variations of a rock or mineral as possible should appear in the
collection, and in many cases examples of the matrix from which the
crystals came. When crystals are tiny, it is well to place them in
vials, that they may not be lost.
Where
Public-domain text, read in full here on John Shaqi.
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