Test: Weathering and Soil Formation - Class 7 MCQ

The three main types of rocks are igneous, metamorphic, and sedimentary. Igneous rocks form from cooled magma or lava, metamorphic rocks arise from existing rocks transformed by heat and pressure, and sedimentary rocks develop from the accumulation and cementation of mineral and organic particles.

The A Horizon, or topsoil, is the layer richest in organic matter and nutrients. It is essential for plant growth as it contains the most active biological activity and fertility compared to the lower horizons.

The primary purpose of soil conservation is to maintain soil health and prevent erosion, which is crucial for sustaining plant life, supporting ecosystems, and ensuring clean water through natural filtration.

Sedimentary rocks are formed from accumulated materials, including the remains of plants and animals. These organic materials can become compacted and cemented over time, forming rocks like coal.

Weathered rock particles constitute the main component of soil. These particles vary depending on the parent rock and are mixed with organic matter, water, and air to create fertile soil.

Mechanical weathering involves the physical breakdown of rocks into smaller pieces without altering their chemical composition. Processes such as ice wedging and abrasion are common examples of mechanical weathering.

While the age of a rock can influence its condition, it is not a direct factor affecting the rate of weathering. In contrast, surface area, climate, and rock type significantly impact how quickly weathering occurs.

Overgrazing leads to soil erosion as plants are removed, leaving soil vulnerable to wind and water. This reduces the soil's ability to retain moisture and nutrients, negatively impacting agriculture and ecosystems.

Chemical weathering refers to the process where rocks undergo chemical reactions that alter their mineral composition. This can include oxidation, hydration, and carbonation, leading to the breakdown of the rock structure.

Cementation is the process through which sediments are compacted and then bonded together by minerals precipitating from water, forming sedimentary rocks. This process occurs typically after sediments have settled in layers.

The parent rock material primarily determines the color of soil. For example, soils derived from red sandstone tend to be reddish due to the iron content, while soils from limestone may appear lighter or grayish.

Coarse-grained igneous rocks, such as granite, form when magma cools slowly underground, allowing large crystals to develop. In contrast, fine-grained rocks, like basalt, form from rapid cooling on the surface.

Metamorphic rocks are formed when existing igneous or sedimentary rocks undergo intense heat and pressure, resulting in a denser and more compact rock. Examples include marble, which originates from limestone.

Eluviation is the process by which fine particles, such as clay, move downward through the soil layers, contributing to soil formation. It contrasts with illuviation, which refers to the accumulation of these particles in lower soil layers.

Soil erosion removes the fertile topsoil necessary for plant growth, leading to decreased plant productivity. This can disrupt ecosystems and reduce agricultural yields, making soil conservation crucial.

Leaching is the process where soluble minerals are washed out from the upper layers of soil to lower layers, often influenced by rainfall. This process can affect soil fertility and nutrient availability.

Afforestation involves planting trees to help hold soil in place with their root systems, which can prevent erosion caused by wind and rain. This method contributes to soil stability and ecosystem health.

Chemical weathering, particularly through carbonation, plays a crucial role in cave formation. Carbonic acid dissolves minerals like calcite in limestone, leading to the development of caves over time.

The type of rock significantly influences the rate of weathering. For instance, quartz-rich rocks weather slowly, while rocks rich in feldspar or calcite weather more quickly due to their chemical composition.

Organic activity, through the decomposition of plants and animals, enriches the soil by mixing organic matter into the top soil layer. This process enhances soil fertility and structure, promoting healthier ecosystems.