HjemGrupperSnakMereZeitgeist
Søg På Websted
På dette site bruger vi cookies til at levere vores ydelser, forbedre performance, til analyseformål, og (hvis brugeren ikke er logget ind) til reklamer. Ved at bruge LibraryThing anerkender du at have læst og forstået vores vilkår og betingelser inklusive vores politik for håndtering af brugeroplysninger. Din brug af dette site og dets ydelser er underlagt disse vilkår og betingelser.

Resultater fra Google Bøger

Klik på en miniature for at gå til Google Books

Indlæser...

Mountains: The origins of the Earth’s mountain systems

af Graham Park

MedlemmerAnmeldelserPopularitetGennemsnitlig vurderingSamtaler
4Ingen3,410,100IngenIngen
'Outstanding Academic Title' Choice, magazine of the Association of College & Research Libraries, American Library Association.Most mountains on Earth occur within relatively well-defined, narrow belts separated by wide expanses of much lower-lying ground. Their distribution is not random but is caused by the now well-understood geological processes of plate tectonics. Some mountains mark the site of a former plate collision - where one continental plate has ridden up over another, resulting in a zone of highly deformed and elevated rocks. Others are essentially volcanic in origin.The most obvious mountain belts today - the Himalayas, the Alps and the Andes, for example - are situated at currently active plate boundaries. Others, such as the Caledonian mountains of the British Isles and Scandinavia, are the product of a plate collision that happened far in the geological past and have no present relationship to a plate boundary. These are much lower, with a generally gentler relief, worn down through millennia of erosion.The presently active mountain belts are arranged in three separate systems: the Alpine-Himalayan ranges, the circum-Pacific belt and the mid-ocean ridges. Much of the Alpine-Himalayan belt is relatively well known, but large parts of the circum-Pacific and ocean-ridge systems are not nearly as familiar, but contain equally impressive mountain ranges despite large parts being partly or wholly submerged.This book takes the reader along the active mountain systems explaining how plate tectonic processes have shaped them, then looks more briefly at some of the older mountain systems whose tectonic origins are more obscure. It is aimed at those with an interest in mountains and in developing an understanding of the geological processes that create them.… (mere)
Ingen
Indlæser...

Bliv medlem af LibraryThing for at finde ud af, om du vil kunne lide denne bog.

Der er ingen diskussionstråde på Snak om denne bog.

Ingen anmeldelser
ingen anmeldelser | tilføj en anmeldelse
Du bliver nødt til at logge ind for at redigere data i Almen Viden.
For mere hjælp se Almen Viden hjælpesiden.
Kanonisk titel
Originaltitel
Alternative titler
Oprindelig udgivelsesdato
Personer/Figurer
Vigtige steder
Vigtige begivenheder
Beslægtede film
Indskrift
Tilegnelse
Første ord
Citater
Sidste ord
Oplysning om flertydighed
Forlagets redaktører
Bagsidecitater
Originalsprog
Canonical DDC/MDS
Canonical LCC

Henvisninger til dette værk andre steder.

Wikipedia på engelsk

Ingen

'Outstanding Academic Title' Choice, magazine of the Association of College & Research Libraries, American Library Association.Most mountains on Earth occur within relatively well-defined, narrow belts separated by wide expanses of much lower-lying ground. Their distribution is not random but is caused by the now well-understood geological processes of plate tectonics. Some mountains mark the site of a former plate collision - where one continental plate has ridden up over another, resulting in a zone of highly deformed and elevated rocks. Others are essentially volcanic in origin.The most obvious mountain belts today - the Himalayas, the Alps and the Andes, for example - are situated at currently active plate boundaries. Others, such as the Caledonian mountains of the British Isles and Scandinavia, are the product of a plate collision that happened far in the geological past and have no present relationship to a plate boundary. These are much lower, with a generally gentler relief, worn down through millennia of erosion.The presently active mountain belts are arranged in three separate systems: the Alpine-Himalayan ranges, the circum-Pacific belt and the mid-ocean ridges. Much of the Alpine-Himalayan belt is relatively well known, but large parts of the circum-Pacific and ocean-ridge systems are not nearly as familiar, but contain equally impressive mountain ranges despite large parts being partly or wholly submerged.This book takes the reader along the active mountain systems explaining how plate tectonic processes have shaped them, then looks more briefly at some of the older mountain systems whose tectonic origins are more obscure. It is aimed at those with an interest in mountains and in developing an understanding of the geological processes that create them.

No library descriptions found.

Beskrivelse af bogen
Haiku-resume

Current Discussions

Ingen

Populære omslag

Quick Links

Vurdering

Gennemsnit: Ingen vurdering.

Er det dig?

Bliv LibraryThing-forfatter.

 

Om | Kontakt | LibraryThing.com | Brugerbetingelser/Håndtering af brugeroplysninger | Hjælp/FAQs | Blog | Butik | APIs | TinyCat | Efterladte biblioteker | Tidlige Anmeldere | Almen Viden | 203,239,922 bøger! | Topbjælke: Altid synlig