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. 2023 Mar 25;9(4):e14866. doi: 10.1016/j.heliyon.2023.e14866

Table 1.

Site characteristics of the pedons in Upper Hoha sub-watershed.

Pedon Geographical position
Altitude (asl) Slope (%) Topographic position Local physiography Parent materials Land use types
Latitude (N) Longitude (E)
1 10°06′14″ 34°33′54.6″ 1577 m 2 Upper slope Convex plateau Residual materials Niger seed farmland
2 10° 07′21.4″ 34°33′58″ 1553 m 3 Upper slope Slightly hilly to the east Weathered basalt rocks Maize farmland
3 10°09′38.3″ 34° 32′51.9″ 1550 m 4 Middle slope Gentle slope Weathered granite rock Maize farmland
4 10°07′47.4″ 34°32′32.5″ 1529 m 2 Middle slope Plain, slopping to the south Residual materials Sorghum farmland
5 10°08′7.9″ 34°34′30.7″ 1524 m 3 Lower slope Gentle slope Residual materials Finger millet farmland
6 10°08′48.6″ 34°32′25.6″ 1494 m 7 Lower slope Slopping to river valley Weathered granite rock Grazing land
7 10 08′44.1″ 34°34′19.1″ 1466 m 1 Toe slope Plain, hilly to the east Colluvic materials Grazing land

Scor. basalt = Scoraceous basalt.