The correct answer is - Tundra is much cooler than deserts, so less water evaporates during the growing season and the tundra stays more moist.
The tundra is a very cold biome. In fact, most of the year is winter, and there is only a short period of time when it is summer, and that is not really a summer in the true sense of the word, as it is relatively cold and fresh.
Since for most of the year the tundra is frozen, the water is not evaporating, and during the very short ''summer'', it defrosts, so it becomes all very marshy, and that allows the plants to grow there.
Also, because the summer so short and relatively cold, the evaporation of the water is minimal, so most of the water just frozen again in the winter.
Answer:
The general pattern in changes in the layers of soil with depth is called <u>Soil Horizon</u>
Explanation:
The layer of soil present parallel to the surface, having different chemical physical and biological properties from the layers that are present above and below it, is known as the soil horizon.
The difference in the properties of the layers of soil can be the texture of the soil, color of the soil, particle size of the soil etc.
Answer:
fertilizers, insecticides and pesticides are washed into water bodies, usually when they are being watered, these fertilizers grow algae and water plants at the surface of the water leaving minimal sunlight and oxygen to reach the marine life, this is called eutrophication.
Explanation:
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1. Tip chernozem.
2. Oaze
3. Acoperirea solului este orice plantă care crește pe o suprafață de pământ.
4. Delta Dunării este cel mai mare parc național
5. Apară adânc. ...
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Folosiți irigarea prin picurare și un cronometru automat.
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Mixează materiale care absorb apa în solul tău.
Answer:
Explanation:
At constructive margins such the mid oceanic ridge where new magma are brought to the surface, evidences abounds to support the theory of continental drift through paleomaganetism.
Continental drift is simply the moving of the land masses on earth from their original positions.
There are certain magnetic minerals in rocks that are able to record the prevailing magnetic conditions in a particular terrane. In a hot magma, at the oceanic ridge for example, these minerals align to the magnetic direction at work during the period when they are cooling. As new materials upwells, the cool layer shifts away from the margin each bearing the paleomagnetic record.
Therefore, through a series of reversals and normality in the magnetic direction, one can deduce that the continents actually moves.
