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The old red sandstone or new walks in an old field / Hugh Miller
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XXVII
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CONTEXTS.

XXVI]

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among the Ancient Rocks contained in this DepositAmazingAbundance of Animal LifeExemplified by a Scene in the Her-ring FisheryPlatform of DeathProbable Cause of the Catas-trophe which rendered it such, . . , 227-240

CHAPTER, XIII.

Successors of the Exterminated TribesThe Gap slowly Filled

Proof that the Vegetation of a Formation may long survive itsAnimal TribesProbable Cause Immensely Extended Periodduring which Fishes were the Master Existences of our PlanetExtreme Folly of an Infidel Objection illustrated by the FactSin-gular Analogy between the History of Fishes as Individuals andas a ClassChemistry of the Lower FormationPrinciples onwhich the Fish -inclosing Nodules were probably FormedChemi-cal Effect of Animal Matter in discharging the Colour from RedSandstoneOrigin of the Prevailing Tint to which the Systemowes its NameSuccessive Modes in which a Metal may exist

The Restorations of the Geologist void of ColourVery DifferentAppearance of the Ichthyolites of Cromarty and Moray, . 241-255

CHAPTER XIV.

The Comstone Formation and its OrganismsDwarf VegetationCcpkalaspidesHuge LobsterHabitats of the Existing Crusta-ceaNo unapt Representation of the Deposit of Balruddery fur-nished by a Land-locked Bay in the Neighbourhood of CromartyVast Space occupied by the Geological FormationsContrast-ed with the Half-formed Deposits which represent the ExistingCreationInferenceThe Formation of the IloloptychiusV ro-bable Origin of its Siliceous LimestoneMarked Increase in theBulk of the Existences of the SystemConjectural CauseTheCoal MeasuresThe Limestone of BurdiehouseConclusion, 256-271

Ichthyolites of the Old Red SandstoneF rom AgassizsPois-sons Fossiles, ...... 272-274