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CHAPTER XXXIV.

THE DIFFERENT AGES OF METAMORPHIC ROCKS.

Difficulty of ascertaining the age of metamorphic strata-The two
schools of metamorphism-Greater accuracy of surveying, and
greater petrological knowledge required-Regional metamorphism
stated to be of different ages, and even to be of Tertiary date by one
school-Stated to be mainly Archæan, and not Post-Palæozoic, by
the other-Regional metamorphism in the Alps, Himalayas, Apen-
nines, and North-west of Scotland-Sameness of hypogene and
regionally metamorphosed rocks

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. 537

STUDENT'S

ELEMENTS OF GEOLOGY.

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-Aërial or Æolian rocks-Volcanic rocks, with and without cones and craters-Plutonic rocks, and their relation to the yolcanic-Metamorphic rocks, and their probable origin-Hypogene

rocks.

Or what materials is the earth composed, and in what manner are these materials arranged? These are the first inquiries with which Geology is occupied, a science which derives its name from the Greek yn, ge, the earth, and Xóyos, logos, a discourse. Previously to experience we might have imagined that investigations of this kind would relate exclusively to the mineral kingdom, and to the various rocks, soils, and metals, which occur upon the surface of the earth, or at various depths beneath it. But, in pursuing such researches, we soon find ourselves led on to consider the successive changes which have taken place in the former state of the earth's surface and interior, and the causes which have given rise to these changes; and, what is still more singular and unexpected, we soon become engaged in researches into the history of the animate creation, or of the various tribes of animals and plants which have, at different periods of the past, inhabited the globe.

All are aware that the solid parts of the earth consist of distinct substances, such as clay, chalk, sand, limestone, coal, slate, granite, and the like; but previously to observation it is commonly imagined that all these have remained from the first in

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