The zone of study is located in the area of Errachidia (south east of Morocco, west of Errachidia city) (Figure 1). The synclinal depression of Goulmima belongs to the furrow pre-African which contains the cretaceous basin of Rheris. It is geographically limited by the High Atlas of Tadighoust and that of Aghbalou N’ kerdous to the north and the west respectively, by Hamada de Meski in the east and the Anti-Atlas in the south  .
The geographical positioning of the zone and the landscape grounds is taken by satellite picture of Google Earth (Figure 2). To have a complete idea, we have proposed to the reader a menu of few photographs emphasized by GIS and MNT (Figure 3).
2. Equipments and Methods
This work exposes the contribution of the GIS and the Digital Model of Ground (MNT) in the study of geomorphological of the selected sites of the area of study  . The MNT
Figure 1. Simplifie geological map of basins of the Wadi Ziz and Wadi Rheris “high central atlas and cretaceous basin of Errachidia” Jarar Oulidi et al., 2005.
Figure 2. Geographical position of the area of study and the geosites (satellite picture of the zone Goulmima-Errachidia (Google Earth)).
Figure 3. Photographs of different landscapes showing the geomorphosites em- phasized by GIS and MNT.
can be obtained by various manners: by scanning and digitalization of topographic cards or by treatment of imagery stereoscopic Radar. In our work, we obtained the MNT via using radar images (SRTM: Shuttle Radar Topography Mission) with a resolution of 90m.
3. Results and Discussion
The MNT makes it possible to individualize well the various geomorphological formations of the zone study. Indeed, the obtained results show two types. Relief of high altitude formed by Turonien of the balcony of ASDRM in yellow color, and the low blue relief represented by the plain of Rheris, formed by quaternary alluvial deposits  (Figure 4). From the MNT, we carried out a synthetic topographic profile of the zone of study (see Figure 5).
The topographic profile realized in the zone area starting from the panoramic landscape of the balcony of ASDRAM, crossing the panoramic landscape of Tifounassine
Figure 4. MNT of Goulmima taken by a radar image SRTM.
Figure 5. Topographic profile across the panoramic landscape of Tifounassine.
towards the chain of high Atlas in Tadighoust This lake morphology is between two reliefs of high altitudes.
The landscape of ASDRM is panoramic when seeing the Oasis of Rheris from a high area. It is good for practising sport (going up and down).
Several cards sets of themes were extracted from the MNT namely: the map of the slopes, orientation, shade and the hydrographic network.
The map of the slopes (Figure 6) shows that the zone is generally characterized by a slope from 20% to 40%. Consequently, the loss of the deposits remains weak at average. It is a preserving zone of these deposits.
The map of orientation (Figure 7) shows:
The reliefs of Turonien and Jurassic show the same north-western direction, while the Oasis and the panoramic landscape of Tifounassine also follow the same south- eastern direction.
The lake Tifounassine and the Oasis of Rheris are considered as receiving zones of the formations subjected to the erosion of the reliefs of secondary age.
Figure 6. Map of the slopes.
Figure 7. Map of orientation.
The map of shade (Figure 8) and visualization in 3D, using tool GIS shows the geomorphology clearly and facilitates their spacial follow-up and their enumeration.
We observe two geomorphological units with light gray and two others with dark gray.
The MNT is subjected to several treatments knowing the realization of the relative layers “flow direction” and consequently the automatic regeneration of the hydrographic network of the zone of study. The comparison with the hydrographic network identified in the topographic cards, shows a good similarity, especially for the boxed wadis (Rheris Wadi)  . The analysis of this network shows two principal directions (Figure 9). First, it is a north-south mountain of Amellagou and Tadighoust. The second direction is west-east of the Wadi El Bour in Tinjdad. The third one is east in Tamda N’messaoud. In fact, these three affluents constitute the Rheris river.
The two first constitute the principal waterways of Atlas origin of the Rheris River which feed the quaternary and infracenomanian ground water and the palm plantation in Goulmima  .
Figure 8. Map of shade.
Figure 9. Map of the hydrographic network.
The use of tool GIS and the image SRTM radar made it possible to have other information sources for understanding the geomorphological aspects of the studied ground well. The MNT made it possible to individualize well the various geomorphological formations with their number, direction… Thus, the current splendid moulding of the landscape has been generated by continued erosion since the Neogene until now. Other information was extracted from the MNT with the edition from the cards sets of themes related to the hydrographic network, the slope, the shade, the model 3D and realization of several topographic profiles. These results, obtained from the development of cartographic documents, facilitate an orientation of the public policies for a better regional planning based on scientific good decisions and a promotion of a possible regional sustainable development.