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Table 1 Relative weights of the each parameter (Wj) and relative weight of different classes (wij) influencing the MM genesis in the province of Tétouan

From: Mass movements susceptibility mapping by using heuristic approach. Case study: province of Tétouan (North of Morocco)

Factors

Relative weight of each parameter (Expert qualitative method) Wj

Class of each parameter

Relative weight of each class (Statistical quantitative method) Wij

Lithology

5

Limestone

1

  

Conglomerates

2

  

Sandstone

3

  

Mudstones

4

  

Marlstones

5

Landuse

5

Buit-up areas

2

  

Forest

3

  

Agriculture

4

  

Bare lands

5

  

Water

1

Fault Density

3

1 - 252m

5

  

252 - 416m

4

  

416 - 583m

3

  

583 - 768m

2

  

768 - 1192m

1

Hydrographic Network Density

2

108 - 1186m

5

  

1186 - 1640m

4

  

1640 - 2038m

3

  

2038 - 2421m

2

  

2421 - 3327m

1

Slope Degrees

4

0−10

1

  

10−20

2

  

20−30

3

  

30−40

4

  

40−50

5

Slope Aspects

1

North (-1 à −71)

5

  

East (71−143)

4

  

NE (143−215)

1

  

South (215−287)

3

  

West (287−359)

2

Elevation

2

0 - 201m

1

  

201 - 436 m

2

  

436 - 706 m

3

  

706 - 1118m

4

  

1118 - 1920m

5