CYCLES OF CHANGE IN THE BRITISH AREA.
Before studying in further detail the strata of the geological column,
it will be convenient to deal with the great physical changes which
have occurred in the British area from Precambrian times to the
present day, as this will clear the way for a right appreciation of
the main variations in the characters and distribution of the strata.
At the end of Precambrian times there was a general upheaval of the
British area, and this we may speak of as the First Continental
Period. It was followed by depression and extensive sedimentation,
proceeding more or less continuously though with local interruptions
through Lower Palæozoic times, so that so far as Britain is concerned
we may speak of Lower Palæozoic times as constituting the First Marine
Period. Extensive upheaval gave rise to continental tracts and
mountain chains, and deposits of abnormal character (as compared with
ordinary marine deposits) at the end of Lower Palæozoic times;--the
Devonian period was one of elevation and denudation, and we may
therefore refer to it as the Second Continental Period. This was
followed by depression and sedimentation in Carboniferous times, and
these Carboniferous times constitute the Second Marine Period.
Elevation gave rise to continental tracts and mountain chains at the
end of Carboniferous times, and here again we find proofs of extensive
denudation and the formation of abnormal deposits:--the Permo-Triassic
period is the Third Continental Period. Depression set in during early
Jurassic times and continued throughout the Mesozoic and the early
part of Tertiary times, which form the Third Marine Period.
Disturbances culminating in Miocene times once more produced
terrestrial conditions. In this, the Fourth Continental Period, we are
still living.
From what has been previously written it will be seen that each of the
marine periods should be marked by an early and late shallow-water
phase, separated by an intervening marine phase, and the importance of
the phases will depend upon the length of time during which they
existed, and will differ markedly in different cases, whilst the
distinctness of the middle phase from the upper and lower, will depend
upon the magnitude of the maximum submergence.
During the first marine period submergence was comparatively rapid,
and the shallow-water phase only lasted through very early Cambrian
times in most regions, whilst the deep-water phase, complicated by
many minor upheavals, extended through the main part of Cambrian,
Ordovician and Silurian times, and was replaced by the later
shallow-water phase at the end of Silurian times.
The second marine period again was ushered in by rapid submergence, so
that the shallow-water phase was brief, and the main mass of the Lower
Carboniferous strata was deposited in deep water; but, unlike the
first marine period, the second was characterised by the occurrence of
a long interval of time marking the later shallow-water phase, during
which the whole of the Upper Carboniferous strata were deposited. The
Carboniferous Marine Period is the simplest of the three with which we
have to deal, as the local oscillations occurring on a fairly large
scale for such movements were less frequent than was the case during
the first and third marine periods.
The third marine period had a long shallow-water phase at the
commencement, with many minor oscillations, causing great variation in
the character of the deposits and frequent minor unconformities. This
shallow-water phase existed throughout Jurassic and Lower Cretaceous
times. The deep-water phase existed during the deposition of the Upper
Cretaceous deposits, and was succeeded by the second shallow-water
phase, when the early Tertiary strata were accumulated.
The difference between the elevations which accompanied the
Continental Periods and those which have been alluded to as minor
elevations is no doubt one of degree, but in considering the British
strata only no confusion is likely to arise on this account, as the
difference was here very great.
The events which occurred during the continental periods are of
extreme importance to the geologist. Every great upheaval was
accompanied by crumpling and stiffening of portions of the earth's
crust, and a definite trend was given to the strata as the result of
these movements. It is to the earth-movements of the four great
continental periods that the present structure of the British Isles is
largely due, and in any attempt to restore the physical history of our
islands considerable attention must be paid to the changes which were
produced in the stratified rocks during these periods of
earth-movement.