The Old Red Sandstone; or, New Walks in an Old Field — John Stuart Mill — John Shaqi
The Old Red Sandstone; or, New Walks in an Old Field
John Stuart Mill · en
CHAPTER IX.
Fossils of the Upper Old Red Sandstone much more imperfectly
preserved than those of the Lower.--The Causes
obvious.--Difference between the two Groups, which first strikes
the Observer, a difference in size.--The _Holoptychius_ a
characteristic Ichthyolite of the Formation.--Description of its
huge Scales.--Of its Occipital Bones, Fins, Teeth, and general
Appearance.--Contemporaries of the _Holoptychius_.--Sponge-like
Bodies.--Plates resembling those of the Sturgeon.--Teeth of
various forms, but all evidently the teeth of fishes.--Limestone
Band and its probable Origin.--Fossils of the Yellow
Sandstone.--the _Pterichthys_ of Dura Den.--Member of a Family
peculiarly characteristic of the System.--No intervening
Formation between the Old Red Sandstone and the Coal
Measures.--The _Holoptychius_ contemporary for a time with the
_Megalichthys_,--The Columns of Tubal-Cain, 151-172
CHAPTER X.
Speculations in the Old Red Sandstone, and their
Character.--George, first Earl of Cromarty.--His Sagacity as
a Naturalist at fault in one instance.--Sets himself to dig
for Coal in the Lower Old Red Sandstone.--Discovers a fine
Artesian Well.--Value of Geological Knowledge in an economic
view.--Scarce a Secondary Formation in the Kingdom in which
Coal has not been sought for.--Mineral Springs of the Old
Red Sandstone.--Strathpeffer.--Its Peculiarities whence
derived.--Chalybeate Springs of Easter Ross and the Black
Isle.--Petrifying Springs.--Building-Stone and Lime of the Old
Red Sandstone.--Its various Soils, 173-189
CHAPTER XI.
Geological Physiognomy.--Scenery of the Primary Formations;
Gneiss, Mica Schist, Quartz Rock.--Of the Secondary; the
Chalk Formations, the Oolite, the New Red Sandstone, the Coal
Measures.--Scenery in the Neighborhood of Edinburgh.--Aspect
of the Trap Rocks.--The Disturbing and Denuding
Agencies.--Distinctive Features of the Old Red Sandstone.--Of
the Great Conglomerate.--Of the Ichthyolite Beds.--The Burn of
Eathie.--The Upper Old Red Sandstones.--Scene in Moray, 190-210
CHAPTER XII.
The two Aspects in which Matter can be viewed; Space and
Time.--Geological History of the Earlier Periods.--The Cambrian
System.--Its Annelids.--The Silurian System.--Its Corals,
Encrinites, Molluscs, and Trilobites.--Its Fish.--These
of a high Order, and called into Existence apparently by
Myriads.--Opening Scene in the History of the Old Red Sandstone
a Scene of Tempest.--Represented by the Great Conglomerate.--Red
a prevailing Color among the Ancient Rocks contained in this
Deposit.--Amazing Abundance of Animal Life.--Exemplified by a
Scene in the Herring Fishery.--Platform of Death.--Probable Cause
of the Catastrophe which rendered it such, 211-225
CHAPTER XIII.