12.07.2015 Views

My life : a record of events and opinions - Wallace-online.org

My life : a record of events and opinions - Wallace-online.org

My life : a record of events and opinions - Wallace-online.org

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

HOME LIFE AND WORK 267including the causes <strong>and</strong> effects <strong>of</strong> the glacial epoch,since these were among the most powerful agents incausing the dispersal <strong>of</strong> all kinds <strong>of</strong> <strong>org</strong>anisms, <strong>and</strong>thus bringing about the actual distribution that nowprevails. This led me to a careful study <strong>of</strong> Mr.James Croll's remarkable works on the subject <strong>of</strong> theastronomical causes <strong>of</strong> glacial <strong>and</strong> interglacial periods,<strong>and</strong> I had much correspondence with him on difficultpoints <strong>of</strong> his theory. While differing on certaindetails, I adopted the main features <strong>of</strong> his theory,combining with it the effects <strong>of</strong> changes in height<strong>and</strong> extent <strong>of</strong> l<strong>and</strong> which form an important adjunctto the meteorological agents. To this subject Idevoted two <strong>of</strong> my longest<strong>and</strong> most argumentativechapters, introducing many considerations not beforetaken account <strong>of</strong>, <strong>and</strong> leading, I still think, to a moresatisfactory explanation <strong>of</strong> the causes that actuallybrought about the glacial epoch than any which havesince been put forth.Besides this partially new theory <strong>of</strong> the causes <strong>of</strong>glacial epochs, the work contained a fuller statement<strong>of</strong> the various kinds <strong>of</strong> evidence proving that thegreat oceanic basins are permanent features <strong>of</strong> theearth's surface, than had before been given ; also adiscussion <strong>of</strong> the mode <strong>of</strong> estimating the durationgeological periods, <strong>and</strong> some considerations<strong>of</strong>leadingto the conclusion that <strong>org</strong>anic change is now lessrapid than the average, <strong>and</strong> therefore that less timeis required for this change than has hitherto beenthought necessary. I was also, I believe, the first topoint out the great differences between the moreancientcontinental isl<strong>and</strong>s <strong>and</strong> those <strong>of</strong> more recentorigin, with the interesting conclusions as to geographicalchanges afforded by both ;while the mostimportant novelty is the theory by which I explained

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!