
The Student's Elements of Geology
- Pages
- about 838
- Category
- Science
- Language
- English
- Reading time
- 15 h at 250 wpm
From the opening
Chapter I—ON THE DIFFERENT CLASSES OF ROCKS.
Geology defined. — Successive Formation of the Earth’s Crust. —
Classification of Rocks according to their Origin and Age. — Aqueous
Rocks. — Their Stratification and imbedded Fossils. — Volcanic Rocks,
with and without Cones and Craters. — Plutonic Rocks, and their
Relation to the Volcanic. — Metamorphic Rocks, and their probable
Origin. — The term Primitive, why erroneously applied to the
Crystalline Formations. — Leading Division of the Work.
Chapter II—AQUEOUS ROCKS—THEIR COMPOSITION AND FORMS OF STRATIFICATION.
Mineral Composition of Strata. — Siliceous Rocks. — Argillaceous. —
Calcareous. — Gypsum. — Forms of Stratification. — Original
Horizontality. — Thinning out. — Diagonal Arrangement. — Ripple-mark.
Chapter III—ARRANGEMENT OF FOSSILS IN STRATA—FRESH-WATER AND MARINE.
Successive Deposition indicated by Fossils. — Limestones formed of
Corals and Shells. — Proofs of gradual Increase of Strata derived from
Fossils. — Serpula attached to Spatangus. — Wood bored by Teredina. —
Tripoli formed of Infusoria. — Chalk derived principally from Organic
Bodies. — Distinction of Fresh-water from Marine Formations. — Genera
of Fresh-water and Land Shells. — Rules for recognising Marine
Testacea. — Gyrogonite and Chara. — Fresh-water Fishes. — Alternation
of Marine and Fresh-water Deposits. — Lym-Fiord.
Chapter IV—CONSOLIDATION OF STRATA AND PETRIFACTION OF FOSSILS.
Chemical and Mechanical Deposits. — Cementing together of Particles. —
Hardening by Exposure to Air. — Concretionary Nodules. — Consolidating
Effects of Pressure. — Mineralization of Organic Remains. — Impressions
and Casts: how formed. — Fossil Wood. — Goppert’s Experiments. —
Precipitation of Stony Matter most rapid where Putrefaction is going
on. — Sources of Lime and Silex in Solution.
Chapter V—ELEVATION OF STRATA ABOVE THE SEA.—HORIZONTAL AND INCLINED
STRATIFICATION.
Why the Position of Marine Strata, above the Level of the Sea, should
be referred to the rising up of the Land, not to the going down of the
Sea. — Strata of Deep-sea and Shallow-water Origin alternate. — Also
Marine and Fresh-water Beds and old Land Surfaces. — Vertical,
inclined, and folded Strata. — Anticlinal and Synclinal Curves.
A short sample. Read the whole book
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