To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

From Wikipedia, the free encyclopedia

Julius Büdel
Born(1903-08-08)8 August 1903
Died28 August 1983(1983-08-28) (aged 80)
NationalityGerman
CitizenshipGermany, West Germany
Alma materUniversity of Vienna
Known forMorphogenetic zones
Relief generations
AwardsAlbrecht-Penck-Medaille (1968)
Victoria Medal (1981)
Scientific career
FieldsClimatic geomorphology
InstitutionsUniversity of Würzburg

Julius Büdel (8 August 1903 – 28 August 1983) was a German geomorphologist noted for his work on the influence of climate in shaping landscapes and landforms.[1] In his work Büdel stressed the importance of inherited landforms in present-day landscapes and argued that many landforms are the result of a combination of processes, and not of a single process.[2] Büdel estimated that 95% of mid-latitude landforms are relict.[3][2] Büdel studied both cold-climate processes in Svalbard and "tropical" weathering processes in India to understand the origin of the relief of Central Europe, which he argued was a palimpsest of landforms formed at different times and under different climates.[2] For Central Europe Büdel concluded that in Late Cretaceous to Early Pliocene times etchplains formed. Then in Late Pliocene to Early Pleistocene times a transition period occurred in landscape forming processes. Finally in the Late Pleistocene periglaciation and deep permafrost made Central Europe a place of "excessive valley cutting". Holocene developments would not have affected much of the landscape other than adding a deep soil cover.[4]

Through his life Büdel published three influential morphoclimatic zoning schemes. The first, in 1948, was followed by another in 1963, and a final version in 1977.[5] Büdel's schemes emphasise planation and valley-cutting in relation to climate, arguing that valley-cutting is dominant in subpolar regions while planation is so in the tropics.[3]

Much of Büdel's 1977 book Klima-geomorphologie was considered outdated as of 2006. However its pioneering approaches make it a classic in geomorphological literature.[2]

The Büdel Islands in Antarctica were named after him.[6]

Morphogenetic zones according to Büdel (1977)
German name[7] English translation[3] Latitude[3] Example[3]
Glacial zone (and immediately adjacent area) 90–65° N
60–90° S
Greenland, Antarctica
Die subpolare Zone exzessiver Talbildung Subpolar zone of excessive valley cutting 80–60° N Canadian Arctic, Taymyr Peninsula
Taiga valley cutting zone, in the permafrost region 70–50° N Russian Far East
Ektropische Zone retardierter Talbildung Ectropic zone of retarded valley cutting 60–35° N
35–55° S
Most of Europe, Patagonia, Eurasian Steppe
Subtropic zone of mixed relief development, etesian region 40–30° N
30–35° S
Morocco, Syria, Central Chile.
Subtropic zone of mixed relief development, monsoonal region 45–25° N
20–40° S
Uruguay, Eastern Cape, South Korea
Die randtropische Zone exzessiver Flächenbildung Peritropical zone of excessive planation 30° N–30° S Venezuela, Angola, Mozambique, Vietnam
Die innertropische Zone partieller Flächenbildung Inter-tropical zone of partial planation 20° N–10° S Panama, Gabon, Sumatra
Warme Trockenzone der Flächenerhaltung und traditionalen Weiterbildung (vorweg durch Sandschwemmebenen) Warm arid zone of surface preservation and traditionally continued development, largely through fluvio-aeolian sandplains 35–10° N
5–30° S
Atacama, Sahara, Thar, Australian Outback
Winterharte Trockenzone der Flächenüberprägung (Transformation) vorweg durch Pedimenteund Glacis Winter cold arid zone of surface transformation, largely through pediments and glacis 50–30° N Gobi, Taklamakan, Maranjab

See also

References

  1. ^ Mensching, Horst G. (1983), "Julius Büdel und sein konzept der klima-geomorphologie – rückschau und würdigung", Erdkunde (in German), 38 (3): 157–166
  2. ^ a b c d Migoń, Piotr (2006). "Büdel, J. 1982: Climatic geomorphology. Princeton: Princeton University Press. (Translation of Klima-geomorphologie, Berlin-Stuttgart: Gebrüder Borntraeger, 1977.)". Progress in Physical Geography. 30 (1): 99–103. doi:10.1191/0309133306pp473xx. S2CID 129512489.
  3. ^ a b c d e Sarre, R.D. (1993). "Climatic geomorphology". In Kearey, Philip (ed.). The Encyclopedia of the Solid Earth Sciences. Blackwell Science Ltd. pp. 112–114. ISBN 978-0-632-03699-8.
  4. ^ Sarre, R.D. (1993). "Climato-genetic geomorphology". In Kearey, Philip (ed.). The Encyclopedia of the Solid Earth Sciences. Blackwell Science Ltd. p. 114. ISBN 978-0-632-03699-8.
  5. ^ Gutiérrez, Mateo; Gutiérrez, Francisco (2013). "Climatic Geomorphology". Treatise on Geomorphology. Vol. 13. pp. 115–131.
  6. ^ Geographic Names Information System of the United States Geological Survey
  7. ^ Klima-Geomorphologie
This page was last edited on 12 October 2023, at 21:49
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.