Nigeria gully erosion crisis
The Nigeria gully erosion crisis has been ongoing since before 1980, and affects communities large and small. It is an ecological, environmental, economic, and humanitarian disaster resulting in land degradation, loss of lives, and properties worth millions of dollars. The estimated number of gullies in the country is at 3,000. They occur due to sandy soil being unable to withstand the runoff and eventually eroding away, leaving gaping gullies that swallow homes and other infrastructure. Gullies and areas exposed to erosion in Southeastern Nigeria tripled from about 1.33% (1,021 km) in 1976 to about 3.7% (2,820  km) in 2006 making the region the most affected region in the country. Causes. Gullies are majorly caused by surface runoff, the erosion occurs, notably, in gullies, which grow wider and deeper with each rainfall. Many of the gullies have become ravines, which can be dozens or hundreds of feet deep. Some natural processes can induce gullies, such as high rainfall, poor soil infiltration and unfavorable catchment shape. The process of gully formation is expedited by the types of soil in Southeastern Nigeria: sandy clay and loamy sand. These are soil types that have greater amounts of sand than clay , loam, or silt. The soil type or texture determines how water flows through it. Soil types with predominantly sandy characteristics allow for pockets of space that water easily moves through. For this reason, sandy soils do not have the ability to hold nutrients and support plant life. Without plants extending their roots into the soil and solidifying it, the chances of soil erosion increase even more. Since erosion plays a large role in soil depletion in this area, it is important to consider fertilization and irrigation when attempting to grow crops. Climate in Nigeria has an extreme impact on the  gully formations. For an area that is predominantly dry, the intensity of the rain often leads to flooding and large amounts of water in one location. The rainfall in Nigeria can be considered aggressive, with large raindrop sizes and high amounts being released at ones. The texture of soil cannot support the water and thus erodes away, and with no vegetation, the process is sped up. However, in Nigeria, the more significant causes of gully formation can be largely attributed to human activities such as: Though concentrated in several towns and states in the south-eastern part of the  country, the crisis affects all Nigerians indirectly. Homes and structures routinely collapse, as the gullies expand with each rainy season. Unchecked, the phenomenon will eventually transform the region into a badland. Topography. The topography of south-eastern Nigeria determines its vulnerability to water erosion. There are three types in the area: plains and lowlands, uplands, and highlands. The highlands, which consist of cuesta landscapes, are resistant to erosion due to their soil composition, but they serve as paths for the water to runoff and erode the lowland areas. A geomorphologist, G. Ofomata, discovered a relationship between the slope of the  hills and the severity of the erosion occurring. On a 15 percent slope, there was a much greater total soil loss than on a compared 1 percent slope. Regardless if they are convex or concave, the sloped lowlands are at risk due to their poor soil characteristics and the angle at which the soil can erode. Impact. There are two levels of impact caused by gully formations: Major interventions. In 2010, President Goodluck Ebele Jonathan made a request to the World Bank Nigeria office for assistance in addressing the challenges of gully erosion, emerging Land degradation and environmental insecurity in  the country. This request resulted in the formation of the Nigeria Erosion and Watershed Management Project (NEWMAP), an eight year multi-sectoral project aimed at addressing gully erosion in the Southern Nigeria and land degradation in the Northern Nigeria. The development objective of the NEWMAP is to reduce vulnerability to soil erosion in targeted sub-watersheds with a portfolio of US$508 million plus an additional financing of $400 million. The Team Leaders of this project are Amos Abu, Ruth Jane Kennedy-Walker and Grant Milne. Before this intervention, several interventions failed to address the challenge of gully erosion  mainly because of inefficiencies in designing proper structures and lack of commitment by the locals to take action. However, in some areas like Madona gully site, Awhum community Enugu State, and Okudu community Imo State, some sustainable interventions base on good practices were employed. These interventions addressed the problem of gully erosion in those areas.