| → enormous 1866 |
| immense 1869 |
| in New Zealand immense 1872 |
|
| → in New Zealand; 1866 1869 |
| OMIT 1872 |
|
| ↑ 2 blocks not present in 1866 1869 1872; present in 1859 1860 1861 |
| South of the equator, we have some direct evidence of former glacial action in New Zealand; and the same plants, found on widely separated mountains in this
island, tell the same story.
If one account which has been published can be trusted, we have direct evidence of glacial action in the south-eastern corner of Australia.
|
|
| → as 1859 1860 1861 1866 |
| of the continent, as 1869 1872 |
|
| → glaciers 1859 1860 1861 1866 |
| nearly under the equator, glaciers 1869 1872 |
|
| → examined 1861 1866 1869 1872 |
| was astonished at the structure of 1859 1860 |
|
| → about 800 feet in height, crossing a valley of the Andes; and this I now feel convinced was a gigantic moraine, left far below any existing glacier. 1859 1860 |
| with great boulders, crossing the Portillo valley, which there can hardly be a doubt once formed a huge moraine; and Mr. D. Forbes informs me that he found in various parts of the Cordillera, from lat. 13° to 30° S., at about the height of 12,000 feet, deeply-furrowed rocks, resembling those with which he was familiar in Norway, and likewise great masses of detritus, including grooved pebbles. 1869 |
| with great boulders, crossing the Portillo valley, which there can hardly be a doubt once formed a huge moraine; and Mr. D. Forbes informs me that he found in various parts of the Cordillera, from lat. 13° to 30° S., at about the height of 12,000 feet, deeply-furrowed rocks, resembling those with which he was familiar in Norway, and likewise great masses of detritus, including grooved pebbles. 1872 |
|
| → former glacial action, in huge boulders transported far from 1866 |
| from 1859 1860 1861 1869 1872 |
|
| ↑ 9 blocks not present in 1859 1860 1861 1866; present in 1869 1872 |
| From these several facts, namely from the glacial action having extended all round the northern and southern hemispheres— from the period having been in a geological sense recent in both hemispheres— from its having lasted in both during a great length of time, as may be inferred from the amount of work effected— and lastly from glaciers having recently descended to a low level along the whole line of the Cordillera, it formerly
appeared to me that we could not avoid the conclusion that the temperature of the whole world had been simultaneously lowered during the Glacial period.
But now Mr. Croll, in a series of admirable memoirs, has attempted to show that a glacial condition of climate is the result of various physical causes, brought into operation by an increase in the excentricity
of the earths
orbit.
All these causes tend towards the same end; but the most powerful appears to be the influence
of the excentricity
of the orbit upon oceanic currents.
It follows from
Mr. Crolls
researches, that
cold periods regularly recur every ten or fifteen thousand years; but that at much longer intervals the cold,
owing to certain contingencies, is extremely severe, and lasts for a great length of time.
Mr. Croll believes that the last great Glacial period occurred about 240,000 years ago, and endured with slight alterations of climate for about 160,000 years.
With respect to more ancient Glacial periods, several geologists are convinced from direct evidence that such occurred during the Miocene and Eocene formations, not to mention still more ancient formations.
But in relation to our present subject,
the most important result arrived
at by Mr. Croll
is,
that whenever the northern hemisphere passes through a cold period, the temperature of the southern hemisphere is actually raised, with the winters rendered much milder, chiefly through changes in the direction of the ocean-currents.
So conversely it is
with the northern hemisphere, when
the southern passes through a glacial period.
These
conclusions
have, as we shall immediately see, a most important bearing
on geographical distribution;
but
I will
first give the facts, which demand an explanation.
|
|
| → formed part of 1866 |
| was included within 1859 1860 1861 |
|
