JAMB UTME - Geography - 2019

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One way to overcome the problem of irregular levels of water in river transport is by building locks and canals. Locks are structures that allow boats and ships to pass from one water level to another. They work by closing and filling with water, which raises or lowers the water level inside the lock to match the water level on the other side. This allows boats and ships to safely navigate through areas where the water level is different. Canals, on the other hand, are man-made waterways that are built to connect two waterways or to bypass a stretch of river with difficult navigational conditions. By providing a controlled and stable water environment, locks and canals can greatly improve the reliability and efficiency of river transport.

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Zambia is a country in Africa that is well-known for its production of copper. Copper is a metal that is widely used in many industries, and Zambia is one of the largest producers of this metal in Africa. In Zambia, copper is extracted from the ground and then processed into different forms, such as wire, pipes, and other products. The mining industry is a major contributor to the economy of Zambia, and the country's copper mines help to provide jobs and support the local economy.

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The igneous rock with distinct grains of mica, feldspar, and quartz is granite. Granite is a type of igneous rock that is formed by the cooling and solidification of magma or lava. It is composed of several minerals, including quartz, feldspar, and mica. These minerals give granite its characteristic speckled appearance and make it a popular choice for building and decorative purposes. Mica is a shiny mineral that appears in thin, flat sheets and gives granite its distinctive glittery look. Feldspar is a group of minerals that are very common in igneous rocks and make up the majority of granite's composition. Quartz is a hard, mineral that is often found in igneous rocks and contributes to granite's durability. In summary, if you find an igneous rock with distinct grains of mica, feldspar, and quartz, it is most likely granite.

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The rocks of the basement complex are generally referred to as older granite. The basement complex is a layer of rock that forms the foundation or base of the Earth's crust. It consists of a variety of igneous and metamorphic rocks that have been deeply buried and intensely deformed over time. The older granite that makes up the basement complex is a type of igneous rock that was formed by the solidification of molten magma deep beneath the Earth's surface. It is typically composed of minerals such as quartz, feldspar, and mica, and is known for its coarse-grained texture and distinctive speckled appearance. The older granite of the basement complex is important because it serves as a stable platform for the overlying sedimentary rocks and volcanic rocks. It also plays a significant role in controlling the location and distribution of mineral deposits, as many valuable ores are associated with the older granite. Overall, the older granite of the basement complex is a fundamental component of the Earth's crust and has significant geological and economic importance.

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A common feature of Forcados, Bonny, and Eket in the Niger Delta is that they are all terminals for oil companies. These three locations are major hubs for the extraction, transportation, and export of crude oil in the region. Forcados, Bonny, and Eket are all situated along the coast of the Niger Delta, which is home to vast reserves of crude oil. Oil companies have established facilities at these locations to extract crude oil from the ground, transport it via pipelines or tankers, and export it to other parts of the world. The oil industry is a crucial part of the economy of the Niger Delta, and Forcados, Bonny, and Eket are all key players in this industry. While fishing is an important activity in the Niger Delta, these locations are not primarily known for their fishing ports. Similarly, while natural gas exports are an important part of the region's economy, Forcados, Bonny, and Eket are not the only locations where this takes place. Finally, while export processing zones do exist in the Niger Delta, this is not a defining characteristic of these three locations.

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The standard time of a country is determined by the longitude of its location on the Earth. A time zone is a region that has the same standard time, and time zones are typically defined as an offset from the Coordinated Universal Time (UTC). In this case, the country has a standard time of GMT + 1 hour, which means it is one hour ahead of the UTC. The longitude that corresponds to this time zone is the one located 15° east of the Prime Meridian, which runs from the North Pole to the South Pole and passes through the Royal Observatory in Greenwich, London, England. So, the local time adopted by the country is 15°E.

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To calculate the birth rate of a country, we need to divide the number of registered births by the total population of the country and then multiply by 100 to get a percentage. In this case, the number of registered births is 3,000,000, and the total population of the country is 150,000,000. So the birth rate is (3,000,000 / 150,000,000) x 100, which simplifies to 2%. Therefore, the answer is%, meaning that the birth rate of the given country is 2%.

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The merging together of a number of urban settlements will produce a conurbation. A conurbation is a region that consists of a cluster of adjacent metropolitan areas and their surrounding suburban and rural areas. It arises when multiple urban settlements grow and expand to the point where they merge and form a single continuous urban area. The resulting conurbation typically has a high population density and can span across several cities or even entire regions. Examples of well-known conurbations include the Greater London area in the UK, the Rhine-Ruhr region in Germany, and the BosWash corridor in the United States.

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The pair of countries where conurbation is most highly developed is USA and England. Conurbation refers to the merging of two or more previously separate cities into a single continuous urban area. This process is most highly developed in the USA and England due to their history of urbanization and industrialization. The cities of London and New York are two of the largest conurbations in the world and serve as centers of finance, commerce, and culture. These cities have grown and expanded over time to include many surrounding suburbs, creating a vast, interconnected metropolitan area.

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Among the options given, the most influential factor in the location of textile and footwear industries is abundant cheap labor. Textile and footwear industries require a large labor force to produce goods at a low cost. If a country has a large supply of labor willing to work for low wages, it can attract textile and footwear industries to set up factories in its territory. This is because labor is usually the largest cost for these industries, and a country with cheap labor can offer cost advantages to manufacturers. Raw materials are also important for these industries, but they can be imported from other countries if they are not available locally. Energy supply and low interest rates may also affect the cost of production, but they are less critical factors than the availability of cheap labor. In summary, countries with a large supply of cheap labor have an advantage in attracting textile and footwear industries because they can offer low production costs to manufacturers, making their products more competitive in the global market.

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The climate described, with a long wet season of up to 10 months, high annual rainfall of 3000mm, and a mean monthly temperature of at least 26°, is most likely a tropical monsoon climate (Am). Tropical monsoon climates are characterized by a distinct dry season and a long, wet season, with most of the precipitation falling during the wet season. The mean monthly temperature in this climate is high, generally above 18°C, and typically exceeds 26°C during the wet season. In contrast, tropical humid (Af) climates are characterized by a year-round high rainfall, with no distinct dry season, and mean monthly temperatures generally above 18°C. Tropical wet and dry (Aw) climates have distinct dry and wet seasons, with the dry season lasting longer than in the monsoon climate. Warm humid subtropical (Cfa) climates have hot summers and cool winters, with precipitation distributed throughout the year. These climates are found in the subtropics and have a mean temperature of at least 10°C in the coldest month.

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In surveying, it is best dealt with by laying offsets. This means that instead of measuring the exact distance or angle to an object that may obstruct the line of sight, the surveyor will measure to a point slightly to the side of the obstruction and then use that measurement to calculate the true distance or angle. This allows the surveyor to gather accurate information without having to physically remove the obstruction or avoid it altogether. By laying offsets, the surveyor can ensure that the survey results are accurate and reliable.

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The best technique to prevent soil erosion in a humid, gently sloping area is contour ridging. Contour ridging involves creating ridges that run along the contour lines of the slope, which helps to slow down the flow of water across the surface of the soil. This technique helps to trap water, reduce its speed, and allow it to penetrate into the soil. By reducing the speed of water, contour ridging also helps to reduce the amount of soil that is carried away by the water, which reduces erosion. Terrace cultivation and intercropping can also be effective techniques for reducing erosion, but they are generally better suited to steeper slopes. Wind breakers can help to reduce erosion caused by wind, but they are not as effective for preventing erosion caused by water. In summary, contour ridging is the best technique for preventing soil erosion in a humid, gently sloping area because it helps to slow down the flow of water and reduce erosion, and it is well-suited to this type of terrain.

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Soil texture is primarily determined by the particle sizes of the mineral components in the soil. These mineral particles can range in size from large rocks to tiny clay particles. The three main particle size classes that determine soil texture are sand, silt, and clay. Sand particles are the largest, ranging in size from 0.05 to 2.0 millimeters. Silt particles are smaller, ranging from 0.002 to 0.05 millimeters. Clay particles are the smallest, less than 0.002 millimeters in size. The proportion of these particle sizes in the soil determines its texture. Soil texture is an important factor that affects many soil properties, including water-holding capacity, drainage, nutrient availability, and the ability of roots to grow. Soil texture is also used as a basis for soil classification, with different textures having different names, such as sandy loam, clay loam, and silty clay.

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The development of climax vegetation in the savannah belt of Nigeria is mainly disturbed by bush burning. This is because frequent burning of the grassland destroys the vegetation cover, which can prevent the establishment of trees and other woody plants that are characteristic of climax vegetation. Bush burning also leads to a reduction in soil nutrients, making it difficult for plants to grow. Although activities such as lumbering, mining, and animal grazing can also contribute to the disturbance of climax vegetation, they are not the main cause. Lumbering and mining, for example, involve the removal of trees and vegetation, but these activities are typically limited in scale and do not occur as frequently as bush burning. Animal grazing can also have an impact on vegetation, but it is usually managed in a way that allows for the recovery of the grassland. Therefore, it is the frequent and uncontrolled practice of bush burning that is the primary cause of disturbance to the development of climax vegetation in the savannah belt of Nigeria.

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Temperature is the weather element that is controlled mainly by latitude. Latitude is a measurement of how far a place is from the equator, with the equator being at 0° latitude and the poles at 90° latitude. The closer a place is to the equator, the more direct sunlight it receives, and the warmer it tends to be. The further away from the equator a place is, the less direct sunlight it receives and the cooler it tends to be. This is why the tropics are warm and the poles are cold. So, in simple terms, latitude mainly affects temperature because it determines the amount of direct sunlight a place receives, which in turn affects its overall temperature.

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A river that enters the sea at a gently inclined costal plain where tidal waves are weak will most likely develop into a delta. A delta is a landform that is formed when a river deposits sediment at its mouth where it meets the sea. The sediment builds up over time, creating a triangular-shaped area that extends into the sea. The gently inclined costal plain and weak tidal waves allow the sediment to accumulate and build up the delta over time. This process can lead to the creation of new land, making the delta a valuable area for agriculture and human settlement.

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The Ruhr coalfield is located in Germany. Specifically, it is located in the western part of the country, in the state of North Rhine-Westphalia. The area is known for its rich deposits of coal and was a major source of coal for Germany during the Industrial Revolution. Today, many of the mines have been closed, but the region still has a strong industrial presence and is home to many factories and businesses.

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The highest category of rural settlement is a village. A village is a small, rural community that typically consists of a group of houses and other buildings, surrounded by farmland. People in a village often have close-knit relationships and rely on each other for support. Villages often have a central area where people gather for social events and activities, such as a village green or town square. Villages may also have basic amenities such as a school, a post office, and a general store. In comparison, a homestead refers to a house and the surrounding land that is used for farming or other agricultural purposes. A hut is a small, simple dwelling, often made of natural materials like mud or thatch. A hamlet is a small settlement, similar to a village, but with a smaller population and fewer amenities.

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The eucalyptus tree is native to Australia and is commonly found in the Australian woodland. Similarly, the teak tree is native to the monsoon forests in Southeast Asia. Just as the eucalyptus is a defining species of the Australian woodland, the teak is a defining species of the monsoon forest.

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A population with low birth and death rates generally presents an aging population structure, meaning there are more older people compared to younger people. This results in an inverted population pyramid, where the base is narrow at the younger ages and wider at the older ages. This occurs because people are living longer and there are fewer newborns to replace them. This population structure has implications for social and economic systems, as it may lead to increased demands for healthcare and pension systems.

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A non-renewable resource is a resource that cannot be easily replenished or regenerated. An example of a non-renewable resource is mineral, such as coal, oil, and natural gas. These resources are formed over millions of years and are finite, meaning they will eventually run out. Unlike renewable resources, like wind and solar power, which can be replenished, non-renewable resources are being consumed faster than they can be replaced. This is why it's important to use these resources wisely and find alternative energy sources to preserve them for future generations.

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Lake Kivu and Lake Malawi are related in that they are both rift valley lakes. Rift valley lakes are formed when tectonic plates move apart, creating a depression that fills with water. Lake Kivu is located in the Albertine Rift, which is part of the East African Rift System, while Lake Malawi is located in the East African Rift. Despite their similarities, the two lakes are located in different parts of the African continent - Lake Kivu is located in Rwanda and the Democratic Republic of Congo, while Lake Malawi is located in Malawi, Tanzania, and Mozambique.

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The most densely populated city which is also the capital of a country in Africa is Cairo, the capital city of Egypt. Cairo is not only the largest city in Egypt but also in the entire African continent, with a population of over 9 million people. It has a very high population density of about 48,000 people per square kilometer, making it one of the most densely populated cities in the world. Cairo is located in the northeastern part of Egypt, along the banks of the River Nile, and it has been the political and cultural center of Egypt for centuries. The city is home to several historical and cultural landmarks such as the Great Sphinx, the Pyramids of Giza, and the Egyptian Museum, which attracts millions of tourists every year. Cairo's population density can be attributed to several factors, including the city's history, economic opportunities, and population growth. The city has experienced significant population growth over the years, with people from rural areas moving to the city in search of employment opportunities and a better quality of life. Additionally, the city's location along the Nile River has also contributed to its high population density, as it has facilitated the growth of agriculture and trade in the region. Overall, Cairo's high population density is a reflection of the challenges faced by many rapidly growing cities in developing countries, including urbanization, lack of adequate infrastructure, and limited resources.

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Urban and rural settlements are differentiated by their function and location. Urban settlements are typically characterized by a high population density and a high level of economic and social activity. They are usually located in or near large cities and serve as centers of commerce, industry, and culture. Urban areas often have a diverse range of amenities and services, including shops, restaurants, entertainment venues, and public transportation. Rural settlements, on the other hand, are typically characterized by a lower population density and a lower level of economic and social activity. They are often located in more remote or isolated areas and serve primarily as centers of agricultural activity. Rural areas may have fewer amenities and services than urban areas, but they often offer a quieter and more natural way of life. In summary, the main differences between urban and rural settlements lie in their function and location. Urban areas are characterized by high population density and a diverse range of economic and social activity, while rural areas are characterized by lower population density and a focus on agricultural activity.

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The Stevenson's screen is a box used to house weather instruments that measure temperature, humidity, and other meteorological variables. It is raised about one meter above the ground to avoid the heat from the ground. When the screen is placed on the ground, it can absorb and radiate heat from the ground, which can affect the accuracy of temperature measurements. By raising it one meter above the ground, the screen is more exposed to the free atmosphere and less affected by the heat from the ground. Additionally, raising the screen helps to reduce the impact of raindrops entering the instruments during heavy rainfall. The height also helps to avoid the effects of nearby trees and other obstacles that could affect wind flow around the instruments and affect the measurements. Therefore, the main reason for raising the Stevenson's screen one meter above the ground is to ensure that the weather instruments inside are measuring the temperature and other meteorological variables accurately and without interference from external factors.

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The group of hardwoods that are suitable for railway sleepers in Nigeria is "mahogamy, obeche, and iroko". These hardwoods are known for their durability and strength, making them ideal for use as railway sleepers which need to withstand the weight of trains and the harsh outdoor environment. Mahogany is a dense and durable hardwood that is known for its strength and resistance to decay, making it a popular choice for railway sleepers. Obeche is a lightweight hardwood with good stability and strength, making it a good choice for railway sleepers that need to be lightweight yet strong. Iroko is a durable hardwood that is resistant to decay and weathering, making it an ideal choice for outdoor use, such as railway sleepers.

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The Harbel Plantation in Liberia is noted for large-scale production of rubber. Rubber is a material made from the sap of rubber trees, which is collected, processed, and turned into various products such as tires, gloves, and rubber bands. The Harbel Plantation is significant because it was one of the first large-scale rubber plantations in Liberia, established in the early 20th century by the Firestone Tire and Rubber Company. The plantation continues to produce rubber to this day and has played an important role in the development of the country's rubber industry.

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Sugar Plantations in Africa are most highly developed in the lowlands of Natal and Mozambique. These two regions have warm climates and fertile soils, which are ideal conditions for growing sugarcane, a plant used to make sugar. The lowlands of Natal and Mozambique are also close to ports, which makes it easier to export the sugar that is produced. Because of these factors, the sugar industry has flourished in these regions, making them the most highly developed areas for sugar production in Africa.

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