Bulletin 3. The flora of the Raritan Formation, 1911 - State of New ...
Bulletin 3. The flora of the Raritan Formation, 1911 - State of New ...
Bulletin 3. The flora of the Raritan Formation, 1911 - State of New ...
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HISTORICA_ SKETCH. 9<br />
IL HISTORICAL SKETCH.<br />
<strong>The</strong> <strong>Raritan</strong> and allied, formations, have been <strong>the</strong> sub)ect <strong>of</strong><br />
numerous contributions to'science during <strong>the</strong> past'fifty years,<br />
while scattered references to <strong>the</strong>se deposits, which extend back<br />
over a century and a half, may be found in <strong>the</strong> older works.<br />
<strong>The</strong> Royal Academy <strong>of</strong> Sciences <strong>of</strong> Sweden sent <strong>the</strong> distinguished<br />
naturalist, Peter Kalm, who is commemorated in <strong>the</strong><br />
generic'name <strong>of</strong> our beautiful laurels (KahniaJ to America, in<br />
t749, and <strong>the</strong> results <strong>of</strong> his travels and investigations were<br />
subsequently published in three volumes at Stockholm, and after-<br />
_vard translated into English and Freffch. His was, perhaps,<br />
<strong>the</strong> first contribution to Coastal Plain geology which is worthy<br />
<strong>of</strong> mention. Twenty-eight years later a German naturalist<br />
Johann David Sehoepf, visited this area, and iu a book published<br />
at Erlangen, ten years later, he records many observations <strong>of</strong><br />
interest. <strong>The</strong> first geologist to attempt any correlation with<br />
Europe was William Maelure, who in various publications covering<br />
<strong>the</strong> period from I8o 9 to 1817, referred <strong>the</strong> Coastal Plain<br />
deposits collectively to <strong>the</strong> "Alluvial formation,' *t_e fourth <strong>of</strong><br />
<strong>the</strong> main divisions <strong>of</strong> Werner's classification.<br />
Samuel Akerly, in i82o, and "James Pierce, in 1823, discussed<br />
<strong>the</strong> "alluvial deposits" in <strong>the</strong> vicinity <strong>of</strong> <strong>Raritan</strong> Bay without,<br />
however, having added much that was new.<br />
<strong>The</strong> 'first author to recognize even in slight measure <strong>the</strong> complexity<br />
<strong>of</strong> <strong>the</strong> Coastal Plain formations was John Finch, an Englishman,<br />
and an ardent collector <strong>of</strong> fossils. He read a paper<br />
before <strong>the</strong> Philadelphia .&cademy in 1824, at <strong>the</strong> dose <strong>of</strong> his<br />
travels, and on <strong>the</strong> eve <strong>of</strong> his departure for England, which was<br />
subsequently published.' Some years later he published a hook<br />
on <strong>the</strong> same subject. He condemns <strong>the</strong> term "alluvial" and<br />
points out that.<strong>the</strong> Coastal Plain deposits o{ Maclure and o<strong>the</strong>rs<br />
are identical with <strong>the</strong> newer Secondary an6 Tertiary _ormations<br />
<strong>of</strong> Europe. <strong>The</strong> non-marine Cretaceous he correlates on <strong>the</strong><br />
Amer. Jour. Sci. (1), NEW VII JERSEY : 31-43, GEOLOGICAL I824. SURVEY