The Tree-line reference article from the English Wikipedia on 24-Jul-2004
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Tree-line

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In this view of an alpine tree-line, the distant line looks particularly sharp.  The foreground shows the transition from trees to no trees.  These trees are stunted and one-sided because of cold and windsEnlarge

In this view of an alpine tree-line, the distant line looks particularly sharp. The foreground shows the transition from trees to no trees. These trees are stunted and one-sided because of cold and winds

Tree-line or timberline is the edge of the habitat at which trees are capable of growing. Beyond the tree-line, they are unable to grow due to inappropriate environmental conditions. There are several types:

At tree-line, tree growth is often very stunted, affected by wind, with the last trees forming low, dense matted bushes. These are known as krummholz, from the German for 'twisted wood'. The tree line, like many other natural lines (lake boundaries, for example), looks sharp from a distance, but upon sufficiently close inspection, it becomes a more gradual transition. Trees grow shorter towards the inhospitable climate until they simply stop growing.

The climate above the tree-line is called an alpine climate. Please see that article for more details on what climatic factors cause trees to fail to grow.

Table of contents
1 Typical tree-line species
2 Table of tree-lines
3 Reference

Typical tree-line species

Some typical tree-line tree species (note the predominance of conifers):

Table of tree-lines

The alpine tree-line at a location is dependent on local variables, such as
aspect of slope and rain shadows. Given this caveat, here is a list of average tree-lines from locations around the globe:
Location Approx. latitude Approx. elevation of tree-line Notes
(m) (ft)
Sweden 68 ° N 400 1300
Swiss Alps 46 ° N 2400 7900
Wyoming, USA 43 ° N 3000 9800
Japanese Alps 39 ° N 2900 9500
Yosemite, USA 38 ° N 3200 10500 Sierra Nevada
Yosemite, USA 38 ° N 3600 11800 Sierra Nevada
Himalayas 28 ° N 4400 14400
Hawaii, USA 20 ° N 2800 9000 precipitation low above the trade winds
Mount Kilimanjaro, Tanzania 3 ° S 3000 9800

Reference

Arno, S. F. & Hammerly, R. P. 1984. Timberline. Mountain and Arctic Forest Frontiers. The Mountaineers, Seattle. ISBN 0-89886-085-7