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Tree line facts for kids

Kids Encyclopedia Facts

The tree-line (or timberline) is the highest or farthest point where trees can grow. Beyond this line, conditions are too harsh for trees to survive. Think of it as an invisible border where the forest stops.

There are different types of tree-lines, each caused by different things:

  • Arctic tree-line: This is the most northern place in the world where trees can grow. Go any farther north, and it's simply too cold for them.
  • Antarctic tree-line: Similar to the Arctic, this is the most southern place where trees can grow. It's also too cold beyond this line.
  • Alpine tree-line: This is the highest point on a mountain where trees can grow. Higher up, it gets too cold, or snow covers the ground for too much of the year. The weather above this line is called an alpine climate.
  • Exposure tree-line: On coasts or lonely mountains, the tree-line can be much lower than in other places. This happens because strong winds make it hard for trees to grow tall.
  • Desert tree-line: In deserts, trees can't grow because there isn't enough rainfall.
  • Toxic tree-line: Sometimes, the ground itself is too dangerous for trees. This can be due to hot lava, steam, acid, or too much salt in the soil. It can also be caused by pollution from humans.
  • Wetland tree-line: This is found near very wet areas like bogs. The ground is so full of water that tree roots can't get enough oxygen to grow. However, some trees, like mangroves, are special and can grow in waterlogged soil.
Jojo-Maly Szyszak 2005
Severe winter weather at the alpine tree-line can make trees grow in a twisted, stunted way. This is called krummholz. Karkonosze, Poland.

At the tree-line, trees often look like low bushes instead of tall trees. If strong winds cause this, these twisted, stunted trees are called krummholz. This German word means 'twisted wood'.

From far away, a tree-line looks like a clear, sharp line. But if you get closer, you'll see that trees just gradually get shorter and shorter until they stop growing completely.

Trees You Find at Tree-lines

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Dahurian Larch trees growing near the Arctic tree-line in Siberia.

Many trees that grow at tree-lines are conifers (trees with needles and cones). Here are some examples:

Alpine Tree-lines Around the World

The exact height of an alpine tree-line changes depending on where it is. Things like the direction a mountain slope faces, whether it's in a rain shadow (a dry area behind a mountain), and how close it is to the geographical pole all play a part.

Here's a table showing the average height of tree-lines in different places around the world:

Location Approx. latitude Approx. elevation of tree-line Notes
(m) (ft)
Sweden 68°N 800 2600
Norway 61°N 1100 3600 Lower near the coast
Swiss Alps 46°N 2100 6900 Higher on the southern side of the Alps.
New Hampshire, USA 44°N 1220 4000 Some peaks have lower tree-lines because of past fires and soil loss.
Wyoming, USA 43°N 3000 9800
Rocky Mountain NP, USA 40°N 3500 11500 On warm southwest slopes; lower (about 2400 m or 8000 ft) on northeast slopes
Japanese Alps 39°N 2900 9500
Yosemite, USA 38°N 3200 10500 West side of Sierra Nevada
Yosemite, USA 38°N 3600 11800 East side of Sierra Nevada
Himalaya 28°N 4400 14400
Hawaii, USA 20°N 2800 9000 Not much rain above the trade winds
Costa Rica 9.5°N 3400 11200
Mount Kilimanjaro, Tanzania 3°S 3000 9800
New Guinea 6°S 3900 12800
Andes, Peru 11°S 3900 12800 East side; on the west side, trees struggle due to dryness.
Sierra de Córdoba, Argentina 31°S 2000 6560 Not much rain above trade winds, also very windy.
Australian Alps, Australia 36°S 2000 6560 West side of Australian Alps
Australian Alps, Australia 36°S 1700 5580 East side of Australian Alps
South Island, New Zealand 43°S 1200 3940 The strong ocean influence makes summers cool, which limits tree growth.

Arctic and Antarctic Tree-lines

Just like alpine tree-lines, the tree-lines near the North and South Poles are affected by local conditions. For example, trees can often grow in river valleys farther north than they could on an open, windy hillside. Ocean currents also play a big role in how far from the equator trees can grow.

Here are some typical polar tree-lines:

Location Approx. longitude Approx. latitude of tree-line Notes
Norway 24°Q 71°N The North Atlantic current makes the Arctic climate here warmer than other coastal places at the same latitude.
West Siberian Plain 75°R 66°N
Central Siberian Plateau 102°S 72°N The extreme continental climate means summers are warm enough for trees to grow at very high latitudes, reaching 72°30'N in the Novaya River valley.
Russian Far East (Kamchatka and Chukotka) 160°E 60°N The Oyashio Current and strong winds keep summer temperatures low, stopping trees from growing. The Aleutian Islands have almost no trees.
Alaska 152°W 68°N Trees grow north on the south-facing slopes of the Brooks Range. The mountains block cold air from the Arctic Ocean.
Northwest Territories, Canada 132°W 69°N Reaches north of the Arctic Circle because of the continental climate and warmer summer temperatures.
Nunavut 95°W 61°N The very cold Hudson Bay pushes the tree-line southward.
Quebec 72°W 56°N The Labrador Current has a very strong effect on summer temperatures. In parts of Labrador, the tree-line goes as far south as 53°N.
Greenland 50°W 64°N There are no native trees here because it's so isolated. A few experimental trees are surviving, but growing slowly, at Søndre Strømfjord, 67°N.
Tierra del Fuego, Chile and Argentina 69°W 55°S Trees grow very close to the southernmost tip of South America. The limit here is more about extreme winds than the climate.
BeagleChannelGlacier
Trees growing along the north shore of the Beagle Channel, 55°S.

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See also

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