Skip to main content

Types of farming

(i) Shifting Cultivation: This is a traditional form of agriculture which is practised in the tropics and subtopics by societies which do not have permanent homes, but moves from one place to another.
(ii) Land rotation: This is a modified form of shifting cultivation. A farmer clears an area of bush, cultivates the land until its fertility decreases, allows it to lie fallow to regain its fertility and then returns to cultivate it again.
    Like shifting cultivation, land rotation is an uneconomical and wasteful farming practice. It cannot provide for the needs of a rapidly growing human population. Often, the land is not left to lie fallow long enough to allow it to regain its fertility before it is cultivated again. This eventually damages the soil and converts the land into into a barren desert. This form of farming is a major factor in the destruction of tropical forests.

(iii) Pastoral Farming: This is a traditional type of farming. Certain tribes keep only grazing livestock such as cattle, sheep and goats. They move with their livestock along the same routes at definite seasons of the year. These routes follow the rain so that the livestock get good grazing land. The routes also avoid areas infested with pests like tsetse flies. In this type of farming, overgrazing of poor pastures may lay the land bare and expose it to soil erosion.
(iv) Crop rotation: In most countries, crop rotation has replaced land rotation and shifting cultivation. Crops in a rotation plan are grown on a piece of land in a particular order and rotated through a three, four, five or six year period. A well closed crop rotation plan will allow the continuous use of land while maintaining soil fertility and controlling pests and diseases at the same time. This farming practice is, there important in the present world where agriculturally suitable land is scarce and the population is large and increasing all the time.

Comments

Popular posts from this blog

Natural soil

 Natural soils are influenced by rainfall and temperature,heavy rain causes the soil to become leached. High temperatures increase the rate of decomposition of organic matter in the soil, thereby lowering its humus content. Thus, climatic conditions tend to produce poor soils in the tropics and rich soils in the temperate regions. Besides climate and vegetation, the parent rock material also contributes to the quality of the soil. For example volcanic rocks tend to produce fertile soils.    Laterite, a red soil which is a product of leaching, is commonly found in the tropics. It is composed mainly of iron and aluminium compounds,and poor in humus and essential plant nutrients, such as phosphorus, nitrogen and potassium. The black and brown soil of the temperate grasslands are the world's richest soils, with a high mineral and humus content. The light coloured desert soils tend to be very rich in minerals but have a low humus content.    Mainly the soils ar...

Rock Formation

A rock may be defined as a hard compact mass made up of cluster of primary or secondary minerals. The primary minerals are those that are as they were made in nature. Some of them are Quartz, Olivine, Pyroxene, Hornblende, Biotite, Muscovite and feldspar. On the other hand, secondary minerals consists of particles worn out from original minerals which have combined with other elements. They exist in form of: (i) Oxide such as those of magnesium, Iron and Aluminum. (ii) Sulphates and carbonates of Iron, Magnesium and Calcium. (iii) Clay minerals such as the silicate clays and the hydrous Oxide.   TYPES OF ROCKS (i) Igneous rock (ii) sedimentary rock (iii) Metamorphic rock. Based on their chemical composition, we have basic and acidic rocks. Granite is a very good example of an acid rock. PROCESSES OF ROCK FORMATION IGNEOUS ROCK :This is formed through the process of cooling and hardening of the molten magma. This molten magna is confined deep down below the earth crust und...

Tin ore

    Tin ore and columbite are two minerals that co-occur in the form of heavy black grains like gunpowder, mixed with sand and gravel. They are deposited in alluvial beds of old river valleys and subsequently buried under layers of soil overburden. The ore is mined by the open cast method. To do this, a powerful machine called a dragline is used to first remove the overburden, and then to scoop out the tin ore which it piles in heaps called a monitor is used to direct a powerful jet of water to this tin wash, which washes it down through a series of sluice boxes. Here, the black, heavy tin grains together with other minerals like columbite, now called tin concentrates, sink to the bottom of the boxes, while the water carries the dirt and sand away.     At this stage, the columbite grains are separated from the pure tin concentrates. The concentrates are then sent to factories to be smelted refined and moulded in bars called tin ingots. It is in the form of either ...