ebooksgratis.com

See also ebooksgratis.com: no banners, no cookies, totally FREE.

CLASSICISTRANIERI HOME PAGE - YOUTUBE CHANNEL
Privacy Policy Cookie Policy Terms and Conditions
Talk:Geography of Iceland - Wikipedia, the free encyclopedia

Talk:Geography of Iceland

From Wikipedia, the free encyclopedia

This article is within the scope of WikiProject Iceland, a WikiProject related to the nation of Iceland. If you would like to participate, you can edit the article attached to this page, or visit the project page, where you can join the project and/or contribute to the discussion.
Start This article has been rated as start-Class on the Project’s quality scale.
(If you rated the article please give a short summary at comments to explain the ratings and/or to identify the strengths and weaknesses.)
Top This article has been rated as top-importance on the importance scale.

Max Naylor 08:58, 2 June 2007 (UTC)

Iceland is the only Nordic country that is not intersected by the Arctic Circle. JIP | Talk 12:31, 19 June 2006 (UTC)

But there are Icelandic islands that are on or north of the arctic circle: Grímsey, Kolbeinsey --Spoon! 04:51, 7 September 2006 (UTC)

[edit] Europe?

Is Iceland in Europe? I guess it is historically and culturally, but physically its closer to North America. Given its location on the mid-Atlantic Ridge, it could be argued it's not actually part of either continent. Rojomoke 23:19, 11 February 2007 (UTC)

To Rojomoke: Geologically, Iceland is part of both; it sits on the ridge that divides the North American plate and the Eurasian plate. But, culturally and politically, they are European because they actually are a Scandinavian country. But you are right that it can be considered not part of either continent, because it IS its own continent; that's right, the ridge is slowing feeding it more and more rocks and it is causing it to expand, and in a few hundred million years, it will be the largest continent on the planet as it grows and the old continents get destroyed. Jabbist (talk) 02:57, 28 February 2008 (UTC)

That is simply not true. Current geological processes are not bound to continue forever. In hundreds of millions of years, the changes will be significant. Divergent zones do not remain divergent indefinitely. Granted, there are many possibilities, and as of now we do not have the capability to project continental drift with certainty, but it is possible that a subduction zone will eventually form off the east coast of North America, effectively ceasing the growth of the Atlantic Ocean. The present day Mid Atlantic Ridge, if its rate of spreading does not meet the rate of subduction, would then be drawn toward the new convergent zone off the east coast. Iceland would then eventually become accreted to the eastern part of North America. During and prior to the assembly of Pangaea, eastern North America was an active plate margin. There are countless exotic terranes representative of this period in geological history throughout the region, that are the result of microcontinents and volcanic island arcs welding to the continent. If billions of years of history are any indication, present day Iceland will be a constituent of another continent in hundreds of millions of years. 152.1.211.29 (talk) 06:14, 28 February 2008 (UTC)

[edit] plagiarism?

looks like a cut and paste from CIA factbook. —Preceding unsigned comment added by TCO (talkcontribs) 12:23, 3 May 2008 (UTC)


aa - ab - af - ak - als - am - an - ang - ar - arc - as - ast - av - ay - az - ba - bar - bat_smg - bcl - be - be_x_old - bg - bh - bi - bm - bn - bo - bpy - br - bs - bug - bxr - ca - cbk_zam - cdo - ce - ceb - ch - cho - chr - chy - co - cr - crh - cs - csb - cu - cv - cy - da - de - diq - dsb - dv - dz - ee - el - eml - en - eo - es - et - eu - ext - fa - ff - fi - fiu_vro - fj - fo - fr - frp - fur - fy - ga - gan - gd - gl - glk - gn - got - gu - gv - ha - hak - haw - he - hi - hif - ho - hr - hsb - ht - hu - hy - hz - ia - id - ie - ig - ii - ik - ilo - io - is - it - iu - ja - jbo - jv - ka - kaa - kab - kg - ki - kj - kk - kl - km - kn - ko - kr - ks - ksh - ku - kv - kw - ky - la - lad - lb - lbe - lg - li - lij - lmo - ln - lo - lt - lv - map_bms - mdf - mg - mh - mi - mk - ml - mn - mo - mr - mt - mus - my - myv - mzn - na - nah - nap - nds - nds_nl - ne - new - ng - nl - nn - no - nov - nrm - nv - ny - oc - om - or - os - pa - pag - pam - pap - pdc - pi - pih - pl - pms - ps - pt - qu - quality - rm - rmy - rn - ro - roa_rup - roa_tara - ru - rw - sa - sah - sc - scn - sco - sd - se - sg - sh - si - simple - sk - sl - sm - sn - so - sr - srn - ss - st - stq - su - sv - sw - szl - ta - te - tet - tg - th - ti - tk - tl - tlh - tn - to - tpi - tr - ts - tt - tum - tw - ty - udm - ug - uk - ur - uz - ve - vec - vi - vls - vo - wa - war - wo - wuu - xal - xh - yi - yo - za - zea - zh - zh_classical - zh_min_nan - zh_yue - zu -