Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco

Mohammed Yazami Ztait; Siham Roudani; Fatima-Zahra Ouali Alami; Abdeslam Taleb; Rachid Laaouidi

doi:doi:10.11648/j.ajma.20210904.11

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Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco

Mohammed Yazami Ztait, Siham Roudani, Fatima-Zahra Ouali Alami, Abdeslam Taleb, Rachid Laaouidi

Published in American Journal of Mechanics and Applications (Volume 9, Issue 4)

Received: 7 March 2022 Accepted: 29 March 2022 Published: 14 April 2022

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Abstract

In this paper, we will study the sedimentary state of the river Sebou, which extends between the Mesopotamia, Inaouene Valley and Bouchabel Valley, which is an area of about 36 km (Figure 1). We will analyze the sedimentary components at the bottom of the oued and the level of the floodplain through the banks of the latter. This area comes directly after the confluence of Oued Sebou with Oued Inaouene, in the area of Hamria in douar Ben Hadan, as it extends to the western borders of the center of Sidi Daoud, downstream of the bridge of Sebou in douar Oulad Ben Hamou, where the Oued Sebou takes a general direction from southeast to northwest. This course draws free river confluences in the floodplain extending to the bottom of the Sebou Valley, which is surrounded by land dominated by clay hills of different heights, and overlooking the valley with long to medium slopes. In our study, we relied on fieldwork, including field observation, identification of sections to be studied and analyzed, determination of the properties of river sediments, including coarse elements and morphometric analysis of the gravel, and we relied on choreographic work to draw crosses. Sections and we worked on the identification of the types of banks and the nature of its sedimentary components, we studied the volume of coarse sedimentary elements, in addition to the study of fine sedimentary materials, including laboratory analysis of micro-sediment grains, and we worked on the morphoscopic analysis of quartz grains.

Published in	American Journal of Mechanics and Applications (Volume 9, Issue 4)
DOI	10.11648/j.ajma.20210904.11
Page(s)	35-45
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Accusative Case, Middle Sebou Valley, Inaouene and Buchable Rivers, Pri- Rif (Morocco)

References

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APA Style

Mohammed Yazami Ztait, Siham Roudani, Fatima-Zahra Ouali Alami, Abdeslam Taleb, Rachid Laaouidi. (2022). Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco. American Journal of Mechanics and Applications, 9(4), 35-45. https://doi.org/10.11648/j.ajma.20210904.11

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ACS Style

Mohammed Yazami Ztait; Siham Roudani; Fatima-Zahra Ouali Alami; Abdeslam Taleb; Rachid Laaouidi. Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco. Am. J. Mech. Appl. 2022, 9(4), 35-45. doi: 10.11648/j.ajma.20210904.11

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AMA Style

Mohammed Yazami Ztait, Siham Roudani, Fatima-Zahra Ouali Alami, Abdeslam Taleb, Rachid Laaouidi. Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco. Am J Mech Appl. 2022;9(4):35-45. doi: 10.11648/j.ajma.20210904.11

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@article{10.11648/j.ajma.20210904.11,
  author = {Mohammed Yazami Ztait and Siham Roudani and Fatima-Zahra Ouali Alami and Abdeslam Taleb and Rachid Laaouidi},
  title = {Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco},
  journal = {American Journal of Mechanics and Applications},
  volume = {9},
  number = {4},
  pages = {35-45},
  doi = {10.11648/j.ajma.20210904.11},
  url = {https://doi.org/10.11648/j.ajma.20210904.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajma.20210904.11},
  abstract = {In this paper, we will study the sedimentary state of the river Sebou, which extends between the Mesopotamia, Inaouene Valley and Bouchabel Valley, which is an area of about 36 km (Figure 1). We will analyze the sedimentary components at the bottom of the oued and the level of the floodplain through the banks of the latter. This area comes directly after the confluence of Oued Sebou with Oued Inaouene, in the area of Hamria in douar Ben Hadan, as it extends to the western borders of the center of Sidi Daoud, downstream of the bridge of Sebou in douar Oulad Ben Hamou, where the Oued Sebou takes a general direction from southeast to northwest. This course draws free river confluences in the floodplain extending to the bottom of the Sebou Valley, which is surrounded by land dominated by clay hills of different heights, and overlooking the valley with long to medium slopes. In our study, we relied on fieldwork, including field observation, identification of sections to be studied and analyzed, determination of the properties of river sediments, including coarse elements and morphometric analysis of the gravel, and we relied on choreographic work to draw crosses. Sections and we worked on the identification of the types of banks and the nature of its sedimentary components, we studied the volume of coarse sedimentary elements, in addition to the study of fine sedimentary materials, including laboratory analysis of micro-sediment grains, and we worked on the morphoscopic analysis of quartz grains.},
 year = {2022}
}

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TY  - JOUR
T1  - Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco
AU  - Mohammed Yazami Ztait
AU  - Siham Roudani
AU  - Fatima-Zahra Ouali Alami
AU  - Abdeslam Taleb
AU  - Rachid Laaouidi
Y1  - 2022/04/14
PY  - 2022
N1  - https://doi.org/10.11648/j.ajma.20210904.11
DO  - 10.11648/j.ajma.20210904.11
T2  - American Journal of Mechanics and Applications
JF  - American Journal of Mechanics and Applications
JO  - American Journal of Mechanics and Applications
SP  - 35
EP  - 45
PB  - Science Publishing Group
SN  - 2376-6131
UR  - https://doi.org/10.11648/j.ajma.20210904.11
AB  - In this paper, we will study the sedimentary state of the river Sebou, which extends between the Mesopotamia, Inaouene Valley and Bouchabel Valley, which is an area of about 36 km (Figure 1). We will analyze the sedimentary components at the bottom of the oued and the level of the floodplain through the banks of the latter. This area comes directly after the confluence of Oued Sebou with Oued Inaouene, in the area of Hamria in douar Ben Hadan, as it extends to the western borders of the center of Sidi Daoud, downstream of the bridge of Sebou in douar Oulad Ben Hamou, where the Oued Sebou takes a general direction from southeast to northwest. This course draws free river confluences in the floodplain extending to the bottom of the Sebou Valley, which is surrounded by land dominated by clay hills of different heights, and overlooking the valley with long to medium slopes. In our study, we relied on fieldwork, including field observation, identification of sections to be studied and analyzed, determination of the properties of river sediments, including coarse elements and morphometric analysis of the gravel, and we relied on choreographic work to draw crosses. Sections and we worked on the identification of the types of banks and the nature of its sedimentary components, we studied the volume of coarse sedimentary elements, in addition to the study of fine sedimentary materials, including laboratory analysis of micro-sediment grains, and we worked on the morphoscopic analysis of quartz grains.
VL  - 9
IS  - 4
ER  -

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Author Information

Mohammed Yazami Ztait

Faculty of Letters and Human Sciences Sais-Fès, University Sidi Mohammed Ben Abdellah, Fez, Morocco
Siham Roudani

Faculty of Social Sciences in Kenitra, Ibn Tofail University, Kenitra, Morocco
Fatima-Zahra Ouali Alami

Faculty of Science and Technology Mohammedia, University Hassan II Casablanca, Casablanca, Morocco
Abdeslam Taleb

Faculty of Science and Technology Mohammedia, University Hassan II Casablanca, Casablanca, Morocco
Rachid Laaouidi

Faculty of Social Sciences in Kenitra, Ibn Tofail University, Kenitra, Morocco

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APA Style

Mohammed Yazami Ztait, Siham Roudani, Fatima-Zahra Ouali Alami, Abdeslam Taleb, Rachid Laaouidi. (2022). Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco. American Journal of Mechanics and Applications, 9(4), 35-45. https://doi.org/10.11648/j.ajma.20210904.11

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ACS Style

Mohammed Yazami Ztait; Siham Roudani; Fatima-Zahra Ouali Alami; Abdeslam Taleb; Rachid Laaouidi. Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco. Am. J. Mech. Appl. 2022, 9(4), 35-45. doi: 10.11648/j.ajma.20210904.11

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AMA Style

Mohammed Yazami Ztait, Siham Roudani, Fatima-Zahra Ouali Alami, Abdeslam Taleb, Rachid Laaouidi. Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco. Am J Mech Appl. 2022;9(4):35-45. doi: 10.11648/j.ajma.20210904.11

Copy | Download

@article{10.11648/j.ajma.20210904.11,
  author = {Mohammed Yazami Ztait and Siham Roudani and Fatima-Zahra Ouali Alami and Abdeslam Taleb and Rachid Laaouidi},
  title = {Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco},
  journal = {American Journal of Mechanics and Applications},
  volume = {9},
  number = {4},
  pages = {35-45},
  doi = {10.11648/j.ajma.20210904.11},
  url = {https://doi.org/10.11648/j.ajma.20210904.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajma.20210904.11},
  abstract = {In this paper, we will study the sedimentary state of the river Sebou, which extends between the Mesopotamia, Inaouene Valley and Bouchabel Valley, which is an area of about 36 km (Figure 1). We will analyze the sedimentary components at the bottom of the oued and the level of the floodplain through the banks of the latter. This area comes directly after the confluence of Oued Sebou with Oued Inaouene, in the area of Hamria in douar Ben Hadan, as it extends to the western borders of the center of Sidi Daoud, downstream of the bridge of Sebou in douar Oulad Ben Hamou, where the Oued Sebou takes a general direction from southeast to northwest. This course draws free river confluences in the floodplain extending to the bottom of the Sebou Valley, which is surrounded by land dominated by clay hills of different heights, and overlooking the valley with long to medium slopes. In our study, we relied on fieldwork, including field observation, identification of sections to be studied and analyzed, determination of the properties of river sediments, including coarse elements and morphometric analysis of the gravel, and we relied on choreographic work to draw crosses. Sections and we worked on the identification of the types of banks and the nature of its sedimentary components, we studied the volume of coarse sedimentary elements, in addition to the study of fine sedimentary materials, including laboratory analysis of micro-sediment grains, and we worked on the morphoscopic analysis of quartz grains.},
 year = {2022}
}

Copy | Download

TY  - JOUR
T1  - Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco
AU  - Mohammed Yazami Ztait
AU  - Siham Roudani
AU  - Fatima-Zahra Ouali Alami
AU  - Abdeslam Taleb
AU  - Rachid Laaouidi
Y1  - 2022/04/14
PY  - 2022
N1  - https://doi.org/10.11648/j.ajma.20210904.11
DO  - 10.11648/j.ajma.20210904.11
T2  - American Journal of Mechanics and Applications
JF  - American Journal of Mechanics and Applications
JO  - American Journal of Mechanics and Applications
SP  - 35
EP  - 45
PB  - Science Publishing Group
SN  - 2376-6131
UR  - https://doi.org/10.11648/j.ajma.20210904.11
AB  - In this paper, we will study the sedimentary state of the river Sebou, which extends between the Mesopotamia, Inaouene Valley and Bouchabel Valley, which is an area of about 36 km (Figure 1). We will analyze the sedimentary components at the bottom of the oued and the level of the floodplain through the banks of the latter. This area comes directly after the confluence of Oued Sebou with Oued Inaouene, in the area of Hamria in douar Ben Hadan, as it extends to the western borders of the center of Sidi Daoud, downstream of the bridge of Sebou in douar Oulad Ben Hamou, where the Oued Sebou takes a general direction from southeast to northwest. This course draws free river confluences in the floodplain extending to the bottom of the Sebou Valley, which is surrounded by land dominated by clay hills of different heights, and overlooking the valley with long to medium slopes. In our study, we relied on fieldwork, including field observation, identification of sections to be studied and analyzed, determination of the properties of river sediments, including coarse elements and morphometric analysis of the gravel, and we relied on choreographic work to draw crosses. Sections and we worked on the identification of the types of banks and the nature of its sedimentary components, we studied the volume of coarse sedimentary elements, in addition to the study of fine sedimentary materials, including laboratory analysis of micro-sediment grains, and we worked on the morphoscopic analysis of quartz grains.
VL  - 9
IS  - 4
ER  -

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