|
|
|
|
| LEADER |
01000caa a22002652 4500 |
| 001 |
JST006604714 |
| 003 |
DE-627 |
| 005 |
20240619152225.0 |
| 007 |
cr uuu---uuuuu |
| 008 |
150323s1944 xx |||||o 00| ||eng c |
| 024 |
7 |
|
|a 10.2307/2421371
|2 doi
|
| 035 |
|
|
|a (DE-627)JST006604714
|
| 035 |
|
|
|a (JST)2421371
|
| 040 |
|
|
|a DE-627
|b ger
|c DE-627
|e rakwb
|
| 041 |
|
|
|a eng
|
| 100 |
1 |
|
|a Hinckley, L. C.
|e verfasserin
|4 aut
|
| 245 |
1 |
4 |
|a The Vegetation of the Mount Livermore Area in Texas
|
| 264 |
|
1 |
|c 1944
|
| 336 |
|
|
|a Text
|b txt
|2 rdacontent
|
| 337 |
|
|
|a Computermedien
|b c
|2 rdamedia
|
| 338 |
|
|
|a Online-Ressource
|b cr
|2 rdacarrier
|
| 520 |
|
|
|a The Davis Mountains are a lava region resulting from deformational movements of late Cretaceous time, later lava flows, and consequent severe erosion. Mount Livermore, the highest point in the group, probably marks the line of a fissure eruption. Early botanical work on the area was done by collectors and descriptive writers; investigations since 1900 have dealt mostly with the ecological phases of botany. Comparison of the records of Fort Davis and McDonald Observatory on Mount Locke indicates an average annual precipitation of at least twenty-five inches on Mount Livermore. The vegetation of the north slope of Mount Livermore is a part of the Petran montane forest. Most of the area belongs to the oak woodland or to various combinations of Pinus-Juniperus-Quercus groupings. Some of the canyons have their own characteristic vegetation.
|
| 650 |
|
4 |
|a Physical sciences
|x Earth sciences
|x Geography
|x Geomorphology
|x Landforms
|x Erosional landforms
|x Canyons
|
| 650 |
|
4 |
|a Biological sciences
|x Biology
|x Botany
|x Dendrology
|x Trees
|x Evergreen trees
|x Conifers
|x Pine trees
|
| 650 |
|
4 |
|a Biological sciences
|x Biology
|x Botany
|x Plant ecology
|x Vegetation
|
| 650 |
|
4 |
|a Physical sciences
|x Earth sciences
|x Geography
|x Geomorphology
|x Topography
|x Sloping terrain
|
| 650 |
|
4 |
|a Biological sciences
|x Biology
|x Botany
|x Plants
|
| 650 |
|
4 |
|a Physical sciences
|x Earth sciences
|x Geography
|x Geomorphology
|x Landforms
|x Tectonic landforms
|x Mountains
|x Ridges
|
| 650 |
|
4 |
|a Biological sciences
|x Ecology
|x Population ecology
|x Synecology
|x Biocenosis
|x Plant communities
|x Forests
|x Coniferous forests
|
| 650 |
|
4 |
|a Physical sciences
|x Earth sciences
|x Geography
|x Geomorphology
|x Landforms
|x Erosional landforms
|x Cliffs
|
| 650 |
|
4 |
|a Biological sciences
|x Biology
|x Botany
|x Dendrology
|x Trees
|
| 650 |
|
4 |
|a Biological sciences
|x Biology
|x Botany
|x Dendrology
|x Shrubs
|
| 655 |
|
4 |
|a research-article
|
| 773 |
0 |
8 |
|i Enthalten in
|t The American Midland Naturalist
|d University of Notre Dame, 1909
|g 32(1944), 1, Seite 236-250
|w (DE-627)332164721
|w (DE-600)2052733-0
|x 19384238
|7 nnns
|
| 773 |
1 |
8 |
|g volume:32
|g year:1944
|g number:1
|g pages:236-250
|
| 856 |
4 |
0 |
|u https://www.jstor.org/stable/2421371
|3 Volltext
|
| 856 |
4 |
0 |
|u https://doi.org/10.2307/2421371
|3 Volltext
|
| 912 |
|
|
|a GBV_USEFLAG_A
|
| 912 |
|
|
|a SYSFLAG_A
|
| 912 |
|
|
|a GBV_JST
|
| 912 |
|
|
|a GBV_ILN_11
|
| 912 |
|
|
|a GBV_ILN_20
|
| 912 |
|
|
|a GBV_ILN_22
|
| 912 |
|
|
|a GBV_ILN_24
|
| 912 |
|
|
|a GBV_ILN_31
|
| 912 |
|
|
|a GBV_ILN_39
|
| 912 |
|
|
|a GBV_ILN_40
|
| 912 |
|
|
|a GBV_ILN_60
|
| 912 |
|
|
|a GBV_ILN_62
|
| 912 |
|
|
|a GBV_ILN_63
|
| 912 |
|
|
|a GBV_ILN_70
|
| 912 |
|
|
|a GBV_ILN_90
|
| 912 |
|
|
|a GBV_ILN_100
|
| 912 |
|
|
|a GBV_ILN_101
|
| 912 |
|
|
|a GBV_ILN_110
|
| 912 |
|
|
|a GBV_ILN_120
|
| 912 |
|
|
|a GBV_ILN_285
|
| 912 |
|
|
|a GBV_ILN_374
|
| 912 |
|
|
|a GBV_ILN_702
|
| 912 |
|
|
|a GBV_ILN_2001
|
| 912 |
|
|
|a GBV_ILN_2003
|
| 912 |
|
|
|a GBV_ILN_2005
|
| 912 |
|
|
|a GBV_ILN_2006
|
| 912 |
|
|
|a GBV_ILN_2009
|
| 912 |
|
|
|a GBV_ILN_2010
|
| 912 |
|
|
|a GBV_ILN_2011
|
| 912 |
|
|
|a GBV_ILN_2014
|
| 912 |
|
|
|a GBV_ILN_2015
|
| 912 |
|
|
|a GBV_ILN_2018
|
| 912 |
|
|
|a GBV_ILN_2020
|
| 912 |
|
|
|a GBV_ILN_2021
|
| 912 |
|
|
|a GBV_ILN_2026
|
| 912 |
|
|
|a GBV_ILN_2027
|
| 912 |
|
|
|a GBV_ILN_2044
|
| 912 |
|
|
|a GBV_ILN_2050
|
| 912 |
|
|
|a GBV_ILN_2057
|
| 912 |
|
|
|a GBV_ILN_2061
|
| 912 |
|
|
|a GBV_ILN_2107
|
| 912 |
|
|
|a GBV_ILN_2190
|
| 912 |
|
|
|a GBV_ILN_2939
|
| 912 |
|
|
|a GBV_ILN_2942
|
| 912 |
|
|
|a GBV_ILN_2946
|
| 912 |
|
|
|a GBV_ILN_2949
|
| 912 |
|
|
|a GBV_ILN_2951
|
| 912 |
|
|
|a GBV_ILN_4012
|
| 912 |
|
|
|a GBV_ILN_4035
|
| 912 |
|
|
|a GBV_ILN_4037
|
| 912 |
|
|
|a GBV_ILN_4046
|
| 912 |
|
|
|a GBV_ILN_4112
|
| 912 |
|
|
|a GBV_ILN_4125
|
| 912 |
|
|
|a GBV_ILN_4126
|
| 912 |
|
|
|a GBV_ILN_4242
|
| 912 |
|
|
|a GBV_ILN_4249
|
| 912 |
|
|
|a GBV_ILN_4251
|
| 912 |
|
|
|a GBV_ILN_4305
|
| 912 |
|
|
|a GBV_ILN_4306
|
| 912 |
|
|
|a GBV_ILN_4307
|
| 912 |
|
|
|a GBV_ILN_4313
|
| 912 |
|
|
|a GBV_ILN_4322
|
| 912 |
|
|
|a GBV_ILN_4323
|
| 912 |
|
|
|a GBV_ILN_4324
|
| 912 |
|
|
|a GBV_ILN_4325
|
| 912 |
|
|
|a GBV_ILN_4335
|
| 912 |
|
|
|a GBV_ILN_4338
|
| 912 |
|
|
|a GBV_ILN_4346
|
| 912 |
|
|
|a GBV_ILN_4367
|
| 912 |
|
|
|a GBV_ILN_4393
|
| 912 |
|
|
|a GBV_ILN_4700
|
| 951 |
|
|
|a AR
|
| 952 |
|
|
|d 32
|j 1944
|e 1
|h 236-250
|