Bedrock-incised gully erosion phenomena on Round Island, Mauritius

Abstract Round Island is a 219 ha volcanic island that lies 22 km north of Mauritius. Reaching almost 300 m in altitude, the small island has steep slopes, thin soils and a rocky coast that dips steeply into the sea. In the past the island has been subjected to human influence through the introduction of alien species, including goats, rabbits and plants, severely degrading the floral and faunal ecology. Since being declared a Nature Reserve in 1957 the rehabilitation of the island has received international praise. However, extensive erosion remains problematic. Unusually, the island exhibits gully forms that extend deeply into the tuff bedrock. A modified version of the Southern African Regional Commission for the Conservation and Utilisation of the Soil (SARCCUS) erosion classification system was used to describe two such bedrock-incised gully networks, ‘camp’ and ‘big’ gully, based on morphometric parameters and erosion severity. Rock hardness was also assessed to determine lithological controls on bedrock-incised erosion features. The gullies have their starting points on the mid-upslope regions as rills. These increase in width and depth downslope to a very severe bedrock-gully erosion classification and an exit at sea level. The predominant rock type on Round Island is tuff which is a relatively weak volcanic rock, as indicated by low mean Schmidt Hammer R-values, implying higher expected bedrock erosion rates. During periods of intense rainfall the bedrock-incised gullies act as transport channels for sediment which is ultimately lost to sea. Rehabilitation efforts entail planting of indigenous species and mechanical soil traps on the slopes which has been effective, although localised. Natural re-vegetation has been occurring in the gully channels, particularly in the mid-sections of the gullies. The most appropriate steps toward rehabilitation should thus focus on the wide-scale establishment of vegetation, as it would appear that due to the extensive nature of gullies on Round Island and its steep topography, erosion is a natural phenomenon that is sensitive to human influence.

[1]  D. O. Wijdenes,et al.  Erosion and sediment transport on steep marly hillslopes, Draix, Haute-Provence, France: an experimental field study , 1998 .

[2]  Javier Casalí,et al.  Ephemeral gully erosion in southern Navarra (Spain) , 1999 .

[3]  J. Boardman,et al.  Development of badlands and gullies in the Sneeuberg, Great Karoo, South Africa , 2003 .

[4]  J. Poesen,et al.  Gully erosion: Impacts, factors and control , 2005 .

[5]  Nancy F. Glenn,et al.  Influence of rock strength on the valley morphometry of Big Creek, central Idaho, USA , 2009 .

[6]  M. E. Dulloo,et al.  Changes in the vegetation and reptile populations on Round Island, Mauritius, following eradication of rabbits , 1994 .

[7]  J. Poesen,et al.  Gully erosion and environmental change: importance and research needs , 2003 .

[8]  J. Poesen,et al.  Gully erosion in dryland environments , 2002 .

[9]  Jesús Álvarez-Mozos,et al.  Accuracy of methods for field assessment of rill and ephemeral gully erosion , 2006 .

[10]  J. Brice Erosion and deposition in the loess-mantled Great Plains, Medicine Creek drainage basin, Nebraska , 1966 .

[11]  G. R. Foster Soil Erosion: Developments in Soil Science 10 , 1983 .

[12]  E. Wohl Bedrock Channel Incision along Piccaninny Creek, Australia , 1993, The Journal of Geology.

[13]  F. Rey Influence of vegetation distribution on sediment yield in forested marly gullies , 2003 .

[14]  J. Poesen,et al.  Medium-term evolution of a gully developed in a loess-derived soil , 2002 .

[15]  W. Dietrich,et al.  Sediment and rock strength controls on river incision into bedrock , 2001 .

[16]  A. C. Imeson,et al.  Gully types and gully prediction. , 1980 .

[17]  A. Teymen,et al.  Determination of mechanical properties of rocks using simple methods , 2008 .

[18]  J. Poesen,et al.  Contribution of gully erosion to sediment production in cultivated lands and rangelands , 1996 .

[19]  Hubert Andrew Ireland,et al.  Principles of Gully Erosion in the Piedmont of South Carolina , 1939 .

[20]  Kate Rowntree,et al.  The relationship between land use and soil erosion in the communal lands near Peddie town, Eastern Cape, South Africa , 2003 .

[21]  Alan D. Howard,et al.  Long Profile Development of Bedrock Channels: Interaction of Weathering, Mass Wasting, Bed Erosion, and Sediment Transport , 2013 .

[22]  M. Selby,et al.  A rock mass strength classification for geomorphic purposes: with tests from Antarctica and New Zealand , 1980, Zeitschrift für Geomorphologie.

[23]  S. Rughooputh,et al.  Mapping of monthly soil erosion risk of mainland Mauritius and its aggregation with delineated basins , 2010 .

[24]  M. Dickson,et al.  The influence of rock resistance on coastal morphology around Lord Howe Island, southwest Pacific , 2004 .

[25]  Kelin X. Whipple,et al.  River incision into bedrock: Mechanics and relative efficacy of plucking, abrasion and cavitation , 2000 .