Audio books & Media Downloads

[ali zi zeperto]

The link does not work any more. could anyone please give a working link?

this book is copyrighted and therefore link doesn`t work anymore.i couldn`t find another one.

[ali zi zeperto]

Hamlet
Author(s): William Shakespeare
Publisher: BBC Audiobooks America
Date : 2005
Quality : Good
Language : English
ISBN-10 : 1932219080

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size : 94.20

[ali zi zeperto]

Michael Jackson - Ein Leben zwischen Black and White
Author(s): Hanspeter Kunzler
Publisher: edel
Date : 2009-07-31
Quality : very good
Language : English
ISBN-10 : 3941674048

part 1-size 95

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part 2 - size : 73

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[seymour]

The link does not work any more. could anyone please give a working link?

this book is copyrighted and therefore link doesn`t work anymore.i couldn`t find another one.

check this [ برای مشاهده لینک ، با نام کاربری خود وارد شوید یا ثبت نام کنید ] ... enjoy.

[ali zi zeperto]

Che Guevara: A Revolutionary Life

Author(s): John Lee Anderson
Language : English
ISBN-10 : 1433270684
ISBN-13 :

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برای مشاهده محتوا ، لطفا وارد شوید یا ثبت نام کنید

برای مشاهده محتوا ، لطفا وارد شوید یا ثبت نام کنید

برای مشاهده محتوا ، لطفا وارد شوید یا ثبت نام کنید

برای مشاهده محتوا ، لطفا وارد شوید یا ثبت نام کنید

برای مشاهده محتوا ، لطفا وارد شوید یا ثبت نام کنید

برای مشاهده محتوا ، لطفا وارد شوید یا ثبت نام کنید

[ali zi zeperto]

Gulliver's Travels
Author(s): Jonathan Swift
Publisher: Blackstone Audio Inc
Date : 2007
Quality : Good
Language : English

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برای مشاهده محتوا ، لطفا وارد شوید یا ثبت نام کنید

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[ali zi zeperto]

The Adventures of Huckleberry Finn
Author(s): Mark Twain
Publisher: BBC Audiobooks America
Date : 2003
Quality : Good
Language : English

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[Sharim]

Hi Friends

I didn't know where can i ask ,so i hope you would help me .

I need an article from Britannica Encyclopedia about : Andean-Type Belts
here :

برای مشاهده محتوا ، لطفا وارد شوید یا ثبت نام کنید

is a summarize of it , but i need full article .

If you have this encyclopedia on your computer and if it is possible please type there Andean-Type Belts and copy its explanation here for me . thanks a lot

[seymour]

Hi Friends

I didn't know where can i ask ,so i hope you would help me .

I need an article from Britannica Encyclopedia about : Andean-Type Belts
here :

برای مشاهده محتوا ، لطفا وارد شوید یا ثبت نام کنید

is a summarize of it , but i need full article .

If you have this encyclopedia on your computer and if it is possible please type there Andean-Type Belts and copy its explanation here for me . thanks a lot

I didn't' get it... what's the summary? ... I didn't find any related material on that page you linked...

can you give us a few lines of the summary...

[Sharim]

yes . you are right
i dont know what happened !!
since yesterday this links was for that summary page . but now it is going to full article page
How ever thanks alot for your attention , the same link goes to something I wanted that

---------- Post added at 05:15 PM ---------- Previous post was at 05:11 PM ----------

Andean-type belts


At some continental margins, is subducted. At some of these sites, the landscape is dominated by volcanoes, such as along the Cascades of western North America or in Japan, but at others, such as along much of the Andes of South America[/URL], volcanoes constitute only a small or even negligible part of the relief. At Andean-type margins, the crust is typically thicker than normal, and high mountains can exist even in the absence of volcanoes. Some of the thickened crust is due to the intrusion of magma from the mantle, and some to crustal shortening.


Oceanic lithosphere is commonly subducted at active continental margins at rates of tens to more than 100 millimetres per year, but crustal shortening within the overriding plate typically occurs at rates of only a few millimetres annually. As at continent-continent collision zones, the crustal shortening occurs both by overthrusting of crystalline terrain onto intact continental crust, which in this case lies landward of the volcanic belt, and by the formation of a fold and thrust belt within sedimentary rock lying on the intact continent. The thrusting of crystalline terrain is probably facilitated by a heating and consequent weakening of the rocks near the volcanoes. The presence or absence of a parallel fold and thrust belt depends in part on the presence or absence of thick sedimentary rocks within which detachment of separate layers can take place.
Notwithstanding large variations in topography and in the style of deformation among Andean belts in general, the scales of deformation and uplift are less than those at collision zones. Overthrust crystalline terrains are smaller, and the crystalline rocks themselves have not been thrust up from depths as great as those at collision zones. Much of the Andes, for instance, consists of sedimentary rock that never was buried deeper than a few kilometres and therefore has not been metamorphosed (heated to high temperature or put under high pressure) or at most only has been mildly metamorphosed. Topography in the high parts of the Andes is typically much gentler than in the Himalayas. The most impressive relief is on the eastern flank of the Andes where rivers responding to a wet climate have cut deep canyons.


Fold and thrust belts can be very well developed at Andean margins. The eastern Cordillera of the Bolivian Andes is an extremely wide fold and thrust belt, but only along the eastern third of the cordillera do simple parallel folds control the topography. Farther west, both the greater role of thrust faulting in the evolution of the cordillera and the longer duration of erosion have diminished the role of folding. Except where rivers have cut deep canyons, relief is not exceptionally great. Similarly while oceanic lithosphere was underthrust beneath the west coast of Canada during the [ برای مشاهده لینک ، با نام کاربری خود وارد شوید یا ثبت نام کنید ] (248,000,000–65,000,000 years ago), the Canadian shield was underthrust more than 200 kilometres beneath the Canadian Rocky Mountains, with crustal shortening occurring by décollement and by folding and thrust faulting within the sedimentary cover.


Thus Andean-type belts have a narrow belt of volcanoes and often a fold and thrust belt on their landward margin. The volcanoes of some belts are built on a high range that is more of a long, narrow plateau than a mountain range, for relief on it is not necessarily great.