October 2021

Percolation is the way in which water moves through solids. Rain seeps into the ground and groundwater flows towards the streams to become surface water or seeps into the underground reservoir, or aquifer. The water then moves through pores within the rock. This process of groundwater movement is called percolation, and it can be observed

There are two types of sedimentary landforms: depositional and erosional. Depositional landforms result from layers of sediment being deposited by water, wind or ice. Erosional features occur when the mechanical actions of glaciers, rivers and waves have removed materials from the earth’s surface, the action having been defined as either “Abrasion” or “Scouring”. 1. Alluvial

There are numerous types of landforms; we’ll be starting with the erosional because they make up the majority of “land.” Erosional landforms include headlands, bays, caves, arches, stacks, stumps and wave-cut platforms. There are also depositional landforms such as beaches, spits and bars. Normally when we think about landforms we think about their shape and

Water flows over the land surface in much the same way as it flows over a carpet, following paths of least resistance. The difference is that water slowly erodes the land where the flow is concentrated. Overland flow tends to be concentrated along roads, railway banks and contours. Depending upon irregularities of the land surface,

Water is one of the most destructive agents in nature. It flows almost everywhere over the land surface, leaving its mark by eroding solids, dissolving minerals, and picking up debris. This running water dissolves rock, picks up soil particles, and carries them downstream as suspended load. It also washes away subsurface soils with tributary gullies

Soil development is the major way in which soil changes with time, but there are other changes that can take place over time. Erosion, forest clearing, and forest succession would be some examples of other ways in which soil could change over time. These processes would all cause a depletion in the top layer unless

There are various factors that influence the formation of soils. For example, the parent material’s role as a basis for soil formation can be discussed as one of the soil forming factors as it is one of the most important factors in the ecological system. Parent material, which consists of mineral and organic materials, provides

Soil forms continuously, but slowly, from the gradual breakdown of rocks through weathering. Soil can be formed in a number of different ways including chemical or physical means which often take place simultaneously. Weathering can be a physical, chemical or biological process: Physical weathering: breakdown of rocks from the result of a mechanical action. Temperature

The deposition of sediment is the natural process by which particles of solid material are transported by wind, water and ice and deposited in a new place. The term deposition can also apply to minerals and salts dissolved in water and carried to places they were not previously present or towards sites where they do