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"alluvial" - 6 õppematerjali

Geography of Madagascar
8
pptx

Geography of Madagascar

Madagascar is an island in the Indian Ocean off the eastern coast of southern Africa, east of Mozambique. At 587,000 square kilometres, Madagascar is the world's 46th-largest country and the fourth- largest island. Madagascar can be divided into five geographical regions: the east coast, the Tsaratanana Massif, the central highlands, the west coast, and the southwest. The east coast The east coast consists of a narrow band of lowlands, formed from the sedimentation of alluvial soils and zone, composed of steep bluffs, alternating with ravines bordering an escarpment of about 500 meters in elevation. The coastline is straight, with the exception of the bay. The east coast is considered dangerous for swimmers and sailors because of the large number of sharks that frequent the shoreline. The Tsaratanana Massif region The island's highest peak, Maromokotro, at 2,876 metres is found in the Tsaratanana Massif, located in the far north of the country.

Geograafia → Inglisekeelne geograafia
3 allalaadimist
Europian Enviromental Database Homework 2018
2
pdf

Europian Enviromental Database Homework 2018

4. Natural eutrophic lakes with Magnopotamion or Hydrocharition -type vegetation 5. Natural dystrophic lakes and ponds 6. Semi-natural dry grasslands and scrubland facies on calcareous substrates (Festuco-Brometalia) (* important orchid sites) 7. Fennoscandian lowland species-rich dry to mesic grasslands 8. Hydrophilous tall herb fringe communities of plains and of the montane to alpine levels 9. Northern boreal alluvial meadows 10. Lowland hay meadows (Alopecurus pratensis, Sanguisorba officinalis) 11. Fennoscandian wooded meadows 12. Active raised bogs 13. Degraded raised bogs still capable of natural regeneration 14. Transition mires and quaking bogs 15. Depressions on peat substrates of the Rhynchosporion 16. Alkaline fens 17. Western Taïga 18. Fennoscandian herb-rich forests with Picea abies 19. Coniferous forests on, or connected to, glaciofluvial eskers

Infoteadus → Andmebaasid ja infootsingud
1 allalaadimist
JUHTIMISE ALUSTE EKSAMIKÜSIMUSED KOOS VASTUSTEGA
13
doc

JUHTIMISE ALUSTE EKSAMIKÜSIMUSED KOOS VASTUSTEGA

korrigeerida iga kõrvalekallet. Inimest huvitavad nii nende kui ka teiste poolt saadavate hüvituste absoluutväärtused. Kui alluv tajub ebaõiglust, siis ta võib: moonutada oma või teiste sisendeid või väljundeid; ajendada teisi muutma nende sisendeid või väljundeid; püüda muuta oma sisendeid või väljundeid; valida teise võrdlusaluse isiku; loobuda, lahkuda.tavaliselt tajuvad alluvad ebaõiglasena saadavat töötasu. Töötasu mõju alluvial oleneb töötasuvormist: ajapalga puhul- ületasustamisel toodab rohkem, kui tasustada õigesti; alatasutamisel toodab vähem ja halvakvaliteediliselt. Tükipalga puhul- ületasustamisel toodab vähem, kuid kõrgekvaliteedilisemalt; alatasustamisel toodab rohkem, kuid madalakvaliteedilisemalt. 26. Kuidas motiveerida inimest Skinneri teooria põhjal. Käitumise muutmise võimalused.

Majandus → Juhtimine
482 allalaadimist
Metsatüübid
16
doc

Metsatüübid

Kasemetsad (kaasikud) on palju tootlikumad kui kuusikud. The undergrowth is rich in species and so is the ground vegetation. The best indicators are goatweed, lungwort, hazelwort, woodruff, dog ´s mercury. The moss layer is sparse and fragmentary. Alusmets on liigirikas, nagu ka alustaimestik. Parimateks indikaatoriteks on: naat, kopsurohi, metspipar, lõhnav varjulill, seljarohi. Samblarinne on hõre ja katkendlik. The fern (Dryopteris) site type occurs in alluvial and synclinal valleys with rivers flowing into and out of them, on leached and saturated gley and peaty soils as well as on fluvisols. Sõnajala (Dryopteris) kasvukohatüüp esineb läbivooluga lammi- ja muldorgudes, leostunud ja küllastunud glei- ja turvastunud muldadel nagu ka lammimuldadel. The major part of trees in the stands consists of grey alder, birch and black alder; the spruce forests can be found in the less swampy or drained part of the site.

Keeled → Inglise keel
93 allalaadimist
Halliste luha taimkatte muutustest
55
pdf

Halliste luha taimkatte muutustest

51. Tamm, L. 1967. Süstaga Halliste jõel. Eesti Loodus 6: 383-386. 52. Taylor, D. R., Aarssen, L. W. & Loehle, C. 1990. The species-pool hypothesis and plant community diversity. Oikos 68: 371-374. 53. Talvi, T., 2001. Pool-looduslikud kooslused. Ökoloogiliste Tehnoloogiate keskus. 54. Tilman, D. 1982. Resource competition and community structure. Princeton University Press, Princeton. 55. Touzard B., Clément B., Lavorel S. 2002. Successional patterns in an eutrophic alluvial wetland of western France. Wetlands 22 (1): 111-125. 56. Truus L., Tõnisson, A. 1998. The ecology of floodplain grasslands in Estonia. In: Joyce CB, Wade PM (eds) European Wet Grasslands: Biodiversity, Management and Restoration. Wiley, Chichester, 49-60. 57. van der Maarel, E. 1998. Species diversity in plant communities in relation to structure and dynamics. In: During H. J., Werger, M.J.A. & Willems, J. H. (eds.). Diversity and

Botaanika → Rakendusbotaanika
2 allalaadimist
Bridges presentation
22
docx

Bridges presentation

they rarely were able to excavate deeply enough to reach hard strata. They had, however, perfected techniques of spread footings - wide timber grillages resting on piles driven into the river bed upon which stone piers were laid. In the foundation of the Rialto Bridge, designer Antonio da Ponte drove six thousand timber piles, capped by three stepped grillages so that the abutment stones could be laid perpendicular to the thrust lines of the arch. Though built on soft alluvial soils, the bridge continues to support a street of jewellery shops enjoyed by tourists four centuries later. The end of the Italian Renaissance witnessed a new vision of bridge construction. More than merely utilitarian, bridges were designed as elegant, grand passage-ways that were part of the visual perspective of the idealized cityscape - major accents to the totally redesigned merchant and capital cities

Keeled → Inglise keel
94 allalaadimist


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