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Bulletin 3. The flora of the Raritan Formation, 1911 - State of New ...

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THE RARITAN FORMATION. 17<br />

/_RAS PERIODS SECTION I_IA'I'ERIALS " BI_21C C_AIIAC.<br />

Quaternary GlaciM products Appearance <strong>of</strong> man<br />

Cenozoic Tertiary Sands and Clays Rise <strong>of</strong> ,_fammals<br />

Cretaceous Sands, Clays and Rise<strong>of</strong> Angiosperms,<br />

Gl_xcouite<br />

Ab_teut<br />

Reptiles TERS<br />

SandslOlle$ alld<br />

Mesozoic Triassic Shales<br />

Extrusive and In- Age <strong>of</strong> Conifers<br />

t_tsi_ i_wR _OWS<br />

Permian Absent Pt eridophytes and<br />

Primitive Seed-<br />

Carboniferous plants <strong>of</strong> <strong>the</strong> Coal<br />

Sandstones, Shales,<br />

De_*otx[au IAmest0nes and Con- Ancestors <strong>of</strong> <strong>the</strong><br />

glomerates Coal Flora .<br />

Paleozoic , Limestones. Shales <strong>The</strong> First Land<br />

Silurian and Sandstones Plants<br />

L{rnesigne S _1_<br />

Ordovician Slates Marine Life<br />

Qal_/brla_ Quartzites and N[ar_ne 1,ire<br />

Limestones<br />

2_<br />

Indications <strong>of</strong> Of<br />

Proterozoic Unknown but very great thickness <strong>of</strong> rocks ganlc Life<br />

Arehmozoic embracing an enormous lapse <strong>of</strong> time<br />

./'3g ,'.--Diagram Showing <strong>the</strong> sequence and reIative thickness <strong>of</strong> <strong>the</strong> Geological<br />

divisions in <strong>New</strong> Jersey.<br />

<strong>of</strong> <strong>the</strong> strata <strong>of</strong> <strong>the</strong> Rarltan formation, and could <strong>the</strong> duration<br />

<strong>of</strong> geological time which has gone before it be expressed in<br />

years, we would obtain a still more vivid picture <strong>of</strong> <strong>the</strong> comparative<br />

youth <strong>of</strong> <strong>the</strong> Cretaceous period, evela though this is <strong>of</strong>fset<br />

with <strong>the</strong> reflection that <strong>the</strong> Cretaceous is removed several million<br />

years from <strong>the</strong> present, ?nd <strong>the</strong> plants described in <strong>the</strong> following<br />

pages antedate all <strong>of</strong> <strong>the</strong> higher animals, and were <strong>the</strong><br />

NEW JERSEY GEOLOGICAL SURVEY

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