Movement of the International Literary Exchanges, between France and North America from January 1845 to May, 1846: With Instructions for Collecting, Preparing, and Forwarding Objects of Natural History Written by The Professors Administrators of The Museum Of Natural History At Paris. And Instructions Relative to Anthropology and Zoology — John Shaqi
Movement of the International Literary Exchanges, between France and North America from January 1845 to May, 1846: With Instructions for Collecting, Preparing, and Forwarding Objects of Natural History Written by The Professors Administrators of The Museum Of Natural History At Paris. And Instructions Relative to Anthropology and Zoology
History
Movement of the International Literary Exchanges, between France and North America from January 1845 to May, 1846: With Instructions for Collecting, Preparing, and Forwarding Objects of Natural History Written by The Professors Administrators of The Museum Of Natural History At Paris. And Instructions Relative to Anthropology and Zoology
Exchange of publications
Basalt beds merit a particular attention, both as regards themselves
and the kind of earth which surrounds or covers them. It must be
noticed if they are divided in irregular masses, tables or prisms, and
what is their arrangement. It be must remarked if they contain the
remains of organised bodies, and care must be taken to take samples in
their different states, also of the matter on which the basalt rests.
It must be certain above all that there is no intervention of
scorified matter, or beds of an earthy appareance, to which the
Germans give the name of Wakke, and which are proved to be of volcanic
origin. The rocks named trachytes by M. Hauey merit the same attention.
They are distinguished above all by primitive porphyries, intermediate
or secondary, by the absence of quartz and the presence of pyroxene or
titanimmed iron.
Whatever may be the nature or age of the soil one sees, it is most
important to collect samples of rocks the most common and most
abundant which constitute the bulk of the soil: the study of the
varieties of subordinate beds and accidental matters of all kind,
should be secondary. In general the appearance of the constitution of
the locality must be considered if one would proceed usfully to
choose the samples destined to represent them; the choice would be
easy if one would establish a rule never to quit a declivity, a
mountain, a country even, without having made the section
(geologically). We should add that these sections should be the
principal object in the labours of the geological traveller.
Too large samples must not be taken, samples of 10 to 8 centimetres,
by 3 or 4 of thickness, are sufficient. Larger samples must not be
taken unless they contain the remains of organic fossils, such as
animal skeletons. To pack these samples, they must be covered with
fine paper; above this paper they will put the ticket or note of
bearing or latitude, then a second fine paper that will be surrounded
with tow, and all will be enveloped in grey paper. These samples will
then be put in a box, placing them upright and in successive beds, as
close together as possible, and filling the interstices with cut paper
or tow, in a way to form a mass that nothing can derange. No space
must be left between the last bed and the cover. The box must be
tarred to avoid humidity.
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