Lake
Ac7_103
Ac7
Cambisols
2 - 5  %
Vertisols
Leptosols
Fluvisols
Calcic
Vertic
Eutric
Cambic
Alluvial /colluvial slopes and outwash fans - Welo
Af4c/v_103
Af4c/v
Andosols
Complexes of eroded residual landforms of low to moderate relief and interspersed fan deposits - Eastern highlands
Rgc_103
Rgc
Luvisols
Major river gorges, canyons and escarpments (may include Rmc etc.)
Rgs_103
Rgs
Nitisols
Luvic
Major river gorges, canyons and escarpments (may include Rms etc.)
Rh2v_103
Rh2v
Nitic
Fluvic
High to mountainous relief hills - Western highlands
Rh3v_103
Rh3v
High to mountainous relief hills - Northeastern  escarpment
Rl2m_103
Rl2m
Low to moderate relief hills - Northern highlands
Rl4v_103
Rl4v
Low to moderate relief hills - Northern escarpment
Rm2v_103
Rm2v
Acrisols
Argic
Moderate to high relief hills - Western highlands
Rw1v_103
Rw1v
Rolling to hilly plateaux - Welega and Ilubabor
Sh4v_103
Sh4v
High to mountainous relief parallel ridge and valley topography associated with extensive fault sets
Shc/g_103
Shc/g
Sm2v_103
Sm2v
Moderate to high relief parallel ridge and valley topography associated with extensive fault sets - Northern highlands
Ab1_104
Ab1
5 - 10  %
Haplic
Basins and depressions with seasonal drainage deficiencies - Central highlands and Sidamo
Ac7_104
Rb2c_104
Rb2c
Dissected lowland plains and low plateaux - Cherher highlands
Rd2c_104
Rd2c
Undulating to rolling lowland plains and low plateaux - Negele and Jijiga
Rgc_104
Rgs_104
Leptic
Rgv_104
Rgv
Major river gorges, canyons and escarpments (may include Rmv, Rhv etc.)
Rh2v_104
Planosols
Rh3v_104
Rjv_104
Rjv
Minor river gorges and ravines
Rl2m_104
Rl4v_104
Rm1s_104
Rm1s
Moderate to high relief hills - Tigray
Rm2c_104
Rm2c
Regosols
Moderate to high relief hills - Eastern high lands and tigray
Rm2v_104
Rm7v_104
Rm7v
Moderate to high relief hills - Northern escarpment
Ru2c_104
Ru2c
Flat to undulating lowland plains and low plateaux - Eastern highlands
Rw1g_104
Rw1g
Rolling to hilly plateaux - Harer
Rw1v_104
Rw4v_104
Rw4v
Rolling to hilly plateaux - Northeastern escarpment
Rxc_104
Rxc
Severely dissected plateaux with moderate relief hills- Welo
Sh4v_104
Shc/g_104
Sm2v_104
Ab1_105
10 - 15 %
Ac7_105
Rb2c_105
Rd2c_105
Rgc_105
Rgs_105
Rgv_105
Rh2v_105
Rh3v_105
Rl2m_105
Rl4v_105
Rm1s_105
Rm2v_105
Rm7v_105
Rmv/s_105
Rmv/s
Moderate to high relief hills - Chercher highlands
Ru2c_105
Rw1v_105
Rw4v_105
Rxc_105
Sh4v_105
Shc/g_105
Sm2v_105
Vs1_105
Vs1
Slightly dissected sideslopes and piedmonts of extinct central volcanoes and other  related forms wi
Ab1_106
15 - 30  %
Ac7_106
Rb2c_106
Rd2c_106
Rgc_106
Rgs_106
Rgv_106
Rh2v_106
Rh3v_106
Rhv/s_106
Rhv/s
High to mountainous relief hills - Chercher highlands
Rl2m_106
Rl4v_106
Rm1s_106
Rm2c_106
Rm2g_106
Rm2g
Moderate to high relief hills - Harer
Rm2v_106
Rm7v_106
Rmv/s_106
Ru2c_106
Rw1v_106
Rw4v_106
Rxc_106
Sh4v_106
Shc/g_106
Sm2v_106
Va2_106
Va2
Afro-alpine plateau summits - Fiche
Vs1_106
Ac7_107
30 - 45  %
Rgc_107
Rgv_107
Rh3v_107
Rhv/s_107
Rm1s_107
Rm7v_107
Rmv/s_107
Rw4v_107
Rxc_107
Sh4v_107
Sm2v_107
Rh3v_108
45 - 60  %
Rm7v_108
Rw1v_202
0.5 - 2 %
Rh2v_203
Gleyic
Rl3v_203
Rl3v
Rm3v_203
Rm3v
Moderate to high relief hills - Northern highlands
Rs1v_203
Rs1v
Severly dissected sideslopes and piedmont zones - Central highlands
Rt1v_203
Rt1v
Moderately dissected sideslopes and piedmont zones - Central highlands
Rw1v_203
Rw2v_203
Rw2v
Rolling to hilly plateaux - Lake Tana
Vq3_203
Vq3
Andic
High volcanic piedmonts and lava plateaux - Debre Marcos
Vz3_203
Vz3
Very  large degraded extinct central volcanoes and volcanic complexes of dramatic mountainous relief
Al1_204
Al1
Lacustrine and fluvio-lacustrine plains - Lake Tana & Abaya
Rb2c_204
Rf1v_204
Rf1v
Undulating sideslopes and piedmont zones strongly influenced by culluvial processes but retaining distinct residual characteristics
Rf6v_204
Rf6v
Rgc_204
Rgv_204
Rh1v_204
Rh1v
High to mountainous relief hills - Central highlands
Rh2v_204
Rh3v_204
Rh4v_204
Rh4v
High to mountainous relief hills - Northern highlands
Rl3v_204
Rm2v_204
Rm3v_204
Rs1v_204
Rt1v_204
Rt2v_204
Rt2v
Moderately dissected sideslopes and piedmont zones - Western highlands
Rw1v_204
Rw2v_204
Ry1v_204
Ry1v
Undulating high plateaux with a substantial proportion of hills interspersed throughout - Western highlands
Sh4v_204
Sm1v_204
Sm1v
Moderate to high relief parallel ridge and valley topography associated with extensive fault sets
Sm2v_204
Ssv_204
Ssv
Steep faulted plain and low plateau complexes of the Ethiopian rift with numerous  fault scraps, sags and associated vents, craters and other volcanic remnants
Vh1_204
Vh1
Degraded extinct central volcanoes, caldera remnants and associated forms of high to mountainous relief
Vj1_204
Vj1
Moderately dissected sideslopes of extinct central volcanoes and other relic volcanic forms, often with small cone and vent remnants
Vq3_204
Vs1_204
Vx1_204
Vx1
Steep severely dissected sideslopes if extinct central volcanoes and other relic volcanic forms, often with small vent and cone remnants
Vz3_204
Ac7_205
Rb2c_205
Rf1v_205
Rf6v_205
Rgc_205
Rgs_205
Rgv_205
Rh1v_205
Rh2v_205
Rh3v_205
Rh4v_205
Rhv/s_205
Rk2v_205
Rk2v
High plateaux with scattered moderate relief hills and substantial areas of seasonal marshland interspersed throughout
Rl3v_205
Rl4v_205
Rm1s_205
Rm1v_205
Rm1v
Moderate to high relief hills - Central highlands
Rm2v_205
Rm3v_205
Rm7v_205
Rp3v_205
Rp3v
Undulating high plateaux - Lake Tana
Rp4v_205
Rp4v
Undulating to rolling high plateaux - Jima and Ambo
Rs1v_205
Rt1v_205
Rt2v_205
Rw1v_205
Rw2v_205
Rxc_205
Ry1v_205
Ryv/s_205
Ryv/s
Undulating high plateaux with a substantial proportion of hills interspersed throughout - Eastern highlands
Sh1v_205
Sh1v
Sh4v_205
Shc/g_205
Sm1v_205
Sm2v_205
Ssv_205
Vh1_205
Vj1_205
Vq3_205
Vx1_205
Vz3_205
Ab1_206
Ac7_206
Rb2c_206
Rd2c_206
Rf1v_206
Rf6v_206
Rgc_206
Rgg_206
Rgg
Major river gorges, canyons and escarpments (may include Rmg, Rhg etc.)
Rgs_206
Rgv_206
Rh1v_206
Rh2v_206
Rh3v_206
Rh4v_206
Rhv/s_206
Rk2v_206
Rl3v_206
Rm1s_206
Rm1v_206
Rm2g_206
Rm2v_206
Rm3v_206
Rm7v_206
Rmv/s_206
Rn2g_206
Rn2g
Hilly plains comprised of undulating plains and low plateaux with a substantial proportion of low to moderate relief hills
Rp4v_206
Rs1v_206
Rt1v_206
Rt2v_206
Ru2c_206
Rw1g_206
Rw1v_206
Rw2v_206
Rxc_206
Ry1v_206
Ryv/s_206
Sh1v_206
Sh4v_206
Shc/g_206
Sm1v_206
Sm2v_206
Sp1v_206
Sp1v
Steep faulted plateaux of the Ethiopian rift margin - Addis Ababa
Ssv_206
Vh1_206
Vj1_206
Vq3_206
Vs1_206
Vx1_206
Vz3_206
Ab1_207
Ac7_207
Rb2c_207
Rd2c_207
Rf1v_207
Rf6v_207
Rgc_207
Rgg_207
Rgs_207
Rgv_207
Rh1v_207
Rh2v_207
Rh3v_207
Rh4v_207
Rhv/s_207
Rm1s_207
Rm1v_207
Rm2g_207
Rm3v_207
Rm7v_207
Rmv/s_207
Rn2g_207
Rs1v_207
Rt2v_207
Rw4v_207
Rxc_207
Ryv/s_207
Sh1v_207
Sh4v_207
Shc/g_207
Sm1v_207
Sm2v_207
Ssv_207
Vh1_207
Vj1_207
Vs1_207
Vx1_207
Vz3_207
Rgc_208
Rgg_208
Rgs_208
Rgv_208
Rh1v_208
Rh2v_208
Rh3v_208
Rh4v_208
Rhv/s_208
Rm1s_208
Rm2g_208
Rm3v_208
Rm7v_208
Rmv/s_208
Rxc_208
Ryv/s_208
Sh1v_208
Sh4v_208
Shc/g_208
Sm2v_208
Sp1v_208
Ssv_208
Vs1_208
Vx1_208
Vz3_208
Rgc_209
>  60  %
Rgv_209
Rh2v_209
Rh3v_209
Rh4v_209
Rhv/s_209
Rm1s_209
Rm7v_209
Rmv/s_209
Rxc_209
Sh4v_209
Vx1_209
Ab1_301
0 - 0.5 %
Ab2_301
Ab2
Basins and depressions with seasonal drainage deficiencies - Western highlands
Ac7_301
Al1_301
As3_301
As3
Mollic
Seasonal swamps and marshes - Highlands and Gambela
Rf1v_301
Rf6v_301
Rgv_301
Rk2v_301
Rm2g_301
Rp3v_301
Rp4v_301
Rpg_301
Rpg
Undulating to rolling high plateaux - Harer
Rq2v_301
Rq2v
Hilly terrain of moderate to high relief with a substantial proportion of moderately sloping valleys interspersed throughout
Rt2v_301
Rw2v_301
Sp1v_301
Vp1_301
Vp1
Phaeozems
Undulating high plateaux formed predominantly on pyroclastic deposits - Central highlands
Vq3_301
Vz3_301
Ab1_302
Ab2_302
Ac7_302
Al1_302
As3_302
Rf1v_302
Rf6v_302
Rgc_302
Rgv_302
Rh3v_302
Rh4v_302
Rjv_302
Rk2v_302
Rl1v_302
Rl1v
Low to moderate relief hills - Central highlands
Rl3v_302
Rl4v_302
Rm2c_302
Rm2g_302
Chromic
Rn2g_302
Rp3v_302
Rp4v_302
Rpg_302
Rq2v_302
Rt2v_302
Rw1g_302
Rw1v_302
Rw2v_302
Ry1v_302
Ryv/s_302
Shc/g_302
Sm2v_302
Sp1v_302
Ssv_302
Vj1_302
Vp1_302
Vq1_302
Vq1
High volcanic piedmonts and lava plateaux - Central highlands
Vq3_302
Vs1_302
Vz3_302
Ab1_303
Pellic
Ab2_303
Ac7_303
Al1_303
As3_303
Rb2c_303
Rd2c_303
Rf1v_303
Rf6v_303
Rgc_303
Rgs_303
Rgv_303
Rh3v_303
Rh4v_303
Rhv/s_303
Rjv_303
Rk2v_303
Rl1v_303
Rl2m_303
Rl3v_303
Rl4v_303
Rm2c_303
Rm2g_303
Rm2v_303
Rm3v_303
Rm7v_303
Rmv/s_303
Rn2g_303
Rp3v_303
Rp4v_303
Rpg_303
Rq2v_303
Rt1v_303
Rt2v_303
Ru2c_303
Rw1g_303
Rw1v_303
Rw2v_303
Rw4v_303
Ry1v_303
Ryv/s_303
Shc/g_303
Sm1v_303
Sm2v_303
Sp1v_303
Ssv_303
Va2_303
Vj1_303
Vp1_303
Vq1_303
Vq3_303
Vs1_303
Ab1_304
Ab2_304
Ac7_304
Al1_304
As3_304
Rb2c_304
Rd2c_304
Rd4c_304
Rd4c
Undulating to rolling lowland plains and low plateaux - Eastern highlands
Rf1v_304
Rf6v_304
Rgc_304
Rgg_304
Rgs_304
Rgv_304
Rh2v_304
Rh3v_304
Rh4v_304
Rhv/s_304
Rjv_304
Rk2v_304
Rl2m_304
Rl3v_304
Rl4v_304
Rm2c_304
Rm2g_304
Rm2v_304
Rm3v_304
Rm7v_304
Rmv/s_304
Rn2g_304
Rp3v_304
Rp4v_304
Rpg_304
Rq2v_304
Rt1v_304
Rt2v_304
Ru2c_304
Rw1g_304
Rw2v_304
Rw4v_304
Rxc_304
Ry1v_304
Ryv/s_304
Sh1v_304
Sh4v_304
Shc/g_304
Sm1v_304
Sm2v_304
Sp1v_304
Ssv_304
Va2_304
Vh1_304
Vj1_304
Vp1_304
Vq1_304
Vq3_304
Vs1_304
Vz3_304
Ab1_305
Ab2_305
Ac7_305
Al1_305
Rb2c_305
Rd2c_305
Rf1v_305
Rgc_305
Rgg_305
Rgs_305
Rgv_305
Rh3v_305
Rh4v_305
Rhv/s_305
Rm1v_305
Rm2c_305
Rm7v_305
Rmv/s_305
Rp4v_305
Rpg_305
Rq2v_305
Rt2v_305
Ru2c_305
Rw1g_305
Rw4v_305
Rxc_305
Ryv/s_305
Sh1v_305
Sh4v_305
Shc/g_305
Sm1v_305
Sp1v_305
Ssv_305
Vh1_305
Vq1_305
Vq3_305
Vs1_305
Ab1_306
Ab2_306
Ac7_306
Rb2c_306
Rf1v_306
Rgc_306
Rgg_306
Rgs_306
Rgv_306
Rh3v_306
Rh4v_306
Rhv/s_306
Rm1s_306
Rm2g_306
Rm7v_306
Rmv/s_306
Rn2g_306
Rp4v_306
Rq2v_306
Rt2v_306
Rw1g_306
Rw4v_306
Rxc_306
Sh1v_306
Shc/g_306
Sm1v_306
Sm2v_306
Sp1v_306
Ssv_306
Vp1_306
Vq3_306
Vs1_306
Rgc_307
Rgg_307
Rgs_307
Rgv_307
Rh3v_307
Rhv/s_307
Rmv/s_307
Rt2v_307
Rxc_307
Shc/g_307
Rm1v_401
Rp3v_401
Rw1v_401
Vp1_401
Rh2v_402
Rjv_402
Rk2v_402
Rm1v_402
Rm3v_402
Rp3v_402
Rs1v_402
Rt1v_402
Rt2v_402
Rw1v_402
Rw2v_402
Rw3v_402
Rw3v
Rolling to hilly plateaux - Central highlands
Ry5v_402
Ry5v
Undulating high plateaux with a substantial proportion of hills interspersed throughout - Central highlands
Ssv_402
Vh1_402
Vj1_402
Vp1_402
Vs1_402
Vx1_402
Vz3_402
Rf1v_403
Rgv_403
Rh2v_403
Rh4v_403
Rjv_403
Rk2v_403
Rl3v_403
Rm1v_403
Rm2g_403
Rm2v_403
Rm3v_403
Rn2g_403
Rp3v_403
Rpg_403
Rs1v_403
Rt1v_403
Rt2v_403
Rw1g_403
Rw1v_403
Rw2v_403
Ry1v_403
Ry5v_403
Ryv/s_403
Sh1v_403
Sp1v_403
Ssv_403
Va2_403
Vh1_403
Vj1_403
Vp1_403
Vq3_403
Vs1_403
Vx1_403
Al1_404
Rb2c_404
Rf1v_404
Rgc_404
Rgs_404
Rgv_404
Rh1v_404
Rh2v_404
Rh4v_404
Rhv/s_404
Rjv_404
Rk2v_404
Rl3v_404
Rm1v_404
Rm2c_404
Rm2g_404
Rm2v_404
Rm3v_404
Rmv/s_404
Rn2g_404
Rp3v_404
Rpg_404
Rs1v_404
Rt1v_404
Rt2v_404
Ru2c_404
Rw1g_404
Rw1v_404
Rw2v_404
Rw3v_404
Ry1v_404
Ry5v_404
Ryv/s_404
Sh1v_404
Shc/g_404
Sp1v_404
Ssv_404
Va2_404
Vh1_404
Vj1_404
Vp1_404
Vq3_404
Vs1_404
Vx1_404
Vz3_404
Rb2c_405
Rd2c_405
Rf1v_405
Rgc_405
Rgg_405
Rgs_405
Rgv_405
Rh1v_405
Rh2v_405
Rh4v_405
Rhv/s_405
Rjv_405
Rk2v_405
Rl3v_405
Rm1v_405
Rm2c_405
Rm2g_405
Rm2v_405
Rm3v_405
Rmv/s_405
Rn2g_405
Rp3v_405
Rpg_405
Rs1v_405
Rt1v_405
Rt2v_405
Ru2c_405
Rw1g_405
Rw1v_405
Rw2v_405
Rw3v_405
Rxc_405
Ry1v_405
Ry5v_405
Ryv/s_405
Sh1v_405
Shc/g_405
Sm1v_405
Sp1v_405
Ssv_405
Va2_405
Vh1_405
Vj1_405
Vp1_405
Vq1_405
Vq3_405
Vs1_405
Vx1_405
Vz3_405
Al3_406
Al3
Lacustrine and fluvio-lacustrine plains - Lake Awassa
Rb2c_406
Rd2c_406
Rf1v_406
Rgc_406
Rgg_406
Rgs_406
Rgv_406
Rh1v_406
Rh2v_406
Rh4v_406
Rhv/s_406
Rjv_406
Rl3v_406
Rm1v_406
Rm2c_406
Rm2g_406
Rm2v_406
Rm3v_406
Rmv/s_406
Rn2g_406
Rs1v_406
Rt1v_406
Rt2v_406
Rw1g_406
Rw1v_406
Rw2v_406
Rw3v_406
Rxc_406
Ry1v_406
Ry5v_406
Ryv/s_406
Sh1v_406
Shc/g_406
Sm1v_406
Sp1v_406
Ssv_406
Vh1_406
Vj1_406
Vp1_406
Vs1_406
Vx1_406
Vz3_406
Rb2c_407
Rgc_407
Rgv_407
Rh1v_407
Rh2v_407
Rh4v_407
Rhv/s_407
Rjv_407
Rm1v_407
Rm2g_407
Rm3v_407
Rmv/s_407
Rt1v_407
Rw1g_407
Rw3v_407
Sh1v_407
Shc/g_407
Ssv_407
Vh1_407
Vp1_407
Vs1_407
Vx1_407
Vz3_407
Rgc_408
Rh1v_408
Rhv/s_408
Rjv_408
Rmv/s_408
Rw3v_408
Ssv_408
Vh1_408
Ab1_501
Rf1v_501
Rk2v_501
Rm2v_501
Rp3v_501
Rt2v_501
Rw1v_501
Vq3_501
Vz3_501
Ab1_502
As3_502
Rf1v_502
Rf6v_502
Rh2v_502
Rh4v_502
Rjv_502
Rk2v_502
Rl1v_502
Rm2v_502
Rm3v_502
Rn2g_502
Rp3v_502
Rq2v_502
Rt2v_502
Rw1v_502
Rw2v_502
Ry1v_502
Vj1_502
Vq3_502
Vz3_502
Ab1_503
Ab2_503
As3_503
Rf1v_503
Rf6v_503
Rgv_503
Rh2v_503
Rh4v_503
Rjv_503
Rk2v_503
Rl1v_503
Rm2g_503
Rm2v_503
Rm3v_503
Rn2g_503
Rp3v_503
Rp4v_503
Rt2v_503
Rw1v_503
Rw2v_503
Ry1v_503
Ryv/s_503
Vj1_503
Vq3_503
Vs1_503
Vz3_503
Ab1_504
Ab2_504
As3_504
Rb2c_504
Rd4c_504
Rf1v_504
Rf6v_504
Rgc_504
Rgg_504
Rgs_504
Rgv_504
Rh1v_504
Rh2v_504
Rh4v_504
Rjv_504
Rk2v_504
Rl1v_504
Rm2v_504
Rm3v_504
Rmv/s_504
Rn2g_504
Rp3v_504
Rp4v_504
Rq2v_504
Rt2v_504
Rw1g_504
Rw1v_504
Rw2v_504
Ry1v_504
Ryv/s_504
Vh1_504
Vj1_504
Vq3_504
Vs1_504
Vx1_504
Vz3_504
Ab2_505
As3_505
Rb2c_505
Rf1v_505
Rf6v_505
Rgc_505
Rgg_505
Rgs_505
Rgv_505
Rh1v_505
Rh2v_505
Rh4v_505
Rjv_505
Rk2v_505
Rl1v_505
Rm2v_505
Rm3v_505
Rmv/s_505
Rn2g_505
Rp4v_505
Rq2v_505
Rt2v_505
Rw1g_505
Rw1v_505
Rw3v_505
Ry1v_505
Ryv/s_505
Sh1v_505
Vh1_505
Vj1_505
Vq3_505
Vs1_505
Vx1_505
Vz3_505
Ab2_506
Al3_506
Rb2c_506
Rf1v_506
Rf6v_506
Rgc_506
Rgg_506
Rgs_506
Rgv_506
Rh1v_506
Rh2v_506
Rh4v_506
Rjv_506
Rm2v_506
Rm3v_506
Rmv/s_506
Rn2g_506
Rp4v_506
Rq2v_506
Rt2v_506
Rw1v_506
Ry1v_506
Ryv/s_506
Sh1v_506
Sm1v_506
Vh1_506
Vj1_506
Vq3_506
Vs1_506
Vx1_506
Vz3_506
Ab2_507
Al3_507
Rgc_507
Rgg_507
Rgs_507
Rgv_507
Rh2v_507
Rh4v_507
Rm2g_507
Rm2v_507
Rn2g_507
Rq2v_507
Rt2v_507
Rw1v_507
Vh1_507
Rgv_508
Rm2v_508
Rgs_603
Rgs_604
Ac7_701
Al1_701
Sm2v_701
Ab1_702
Ac7_702
Al1_703
Rhodic
Rm2g_704
Rm2g_705
Rm2g_706
Shc/g_804
Rgc_805
Rgc_906
Calcisols
Rh2v_1101
Rw1v_1101
Rh2v_1102
Rw1v_1102
Rh2v_1103
Rw1v_1103
Rh2v_1104
Rh2v_1105
Rh2v_1106
Rw1v_1202
Gleysols
Vp1_1302