1-10 OF 10 RESULTS FOR

Raidak-I River

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 February 2023
Jour. Geol. Soc. India (2023) 99 (2): 247–258.
... wavelength (L m ), meander amplitude and meander belt width are measured on GIS platform at five meander loops along the lower stretch of river Raidak-I. The conceptual model of different properties of meander is presented in Fig. 2b . Radius of curvature (Rc) has been measured by using the method formerly...
FIGURES | View All (9)
Image
Different phases of neck cutoff formation of river Raidak-I (1955-2019) near village Dhalpal in Tufanganjj-I block of Cooch Behar district. Red rectangle denotes the location of cutoffs.
Published: 01 February 2023
Fig.3. Different phases of neck cutoff formation of river Raidak-I (1955-2019) near village Dhalpal in Tufanganjj-I block of Cooch Behar district. Red rectangle denotes the location of cutoffs.
Image
Different phases of neck cutoff formation of river Raidak-I (1955-2019) near village Bashraja Pratham Khanda. Red rectangle denotes cutoff site located 2.10 km downstream from village Bashraja Pratham Khanda in Tufanganj-I block of Cooch Behar district.
Published: 01 February 2023
Fig.4. Different phases of neck cutoff formation of river Raidak-I (1955-2019) near village Bashraja Pratham Khanda. Red rectangle denotes cutoff site located 2.10 km downstream from village Bashraja Pratham Khanda in Tufanganj-I block of Cooch Behar district.
Image
(a) Flood season discharge of river Raidak-I (from June to September) at Chepan L.R.P crossing river gauge station, Alipurduar (2000-2007); (b) A conceptual model showing different properties of a meander belt.
Published: 01 February 2023
Fig.2. (a) Flood season discharge of river Raidak-I (from June to September) at Chepan L.R.P crossing river gauge station, Alipurduar (2000-2007); (b) A conceptual model showing different properties of a meander belt.
Image
(a) Quaternary sedimentary bank facies along the left bank of an abandoned reach of river Raidak-I near Bashraja Pratham Khanda village in Tufanganj-II block of Cooch Behar district; field photograph showing the different layers of an exposed bank facies; (b) Another sedimentary bank facies along the left bank of an abandoned channel near Begarkhata village in Tufanganj-II block of Cooch Behar; field photograph showing four sedimentary layers of vulnerable bank facies; Field photographs of different abandoned channel as observed near (c) Dhalpal; (d) Bashraja Pratham Khanda; (e) Tufanganj; (f) Begarkhata and (g) Debgram along the lower reach of river Raidak-I.
Published: 01 February 2023
Fig.9. (a) Quaternary sedimentary bank facies along the left bank of an abandoned reach of river Raidak-I near Bashraja Pratham Khanda village in Tufanganj-II block of Cooch Behar district; field photograph showing the different layers of an exposed bank facies; (b) Another sedimentary bank
Image
Study area map shows present cutoffs location and future cutoffs site within the study reach of the river Raidak-I in Alipurduar and Cooch Behar district of West Bengal, India.
Published: 01 February 2023
Fig.1. Study area map shows present cutoffs location and future cutoffs site within the study reach of the river Raidak-I in Alipurduar and Cooch Behar district of West Bengal, India.
Image
Different phases of neck cutoff formation (1955-2019) near village Debgram in Tufanganj-II block of Cooch Bihar district. Red rectangle denotes the location of cutoff-5 which is located 8 km upstream from confluence site of river Raidak-I at Balabhut.
Published: 01 February 2023
Fig.7. Different phases of neck cutoff formation (1955-2019) near village Debgram in Tufanganj-II block of Cooch Bihar district. Red rectangle denotes the location of cutoff-5 which is located 8 km upstream from confluence site of river Raidak-I at Balabhut.
Journal Article
Published: 01 October 2018
Jour. Geol. Soc. India (2018) 92 (4): 441–448.
... is known for its frequent channel shifts ( Hazarika et al., 2015 ). The river experienced major shift in its bankline during the floods of 1988. Levee crevassing and avulsions are common in Simen ( Fig. 2b i-ii ). In a recent avulsion which took place near Somkong in 2013, Simen captured Narad river...
FIGURES | View All (5)
Journal Article
Published: 01 October 2024
Jour. Geol. Soc. India (2024) 100 (10): 1466–1476.
... which indicate the spatial and temporal variation of the centerline of the Mahaweli River. Equations 1, 2, and 3 present the formulations for centerline arc-length (s i ), inflection angle (θ i ), and curvature (c i ) at two successive points. More information on these formulations can be found...
FIGURES | View All (9)
Journal Article
Published: 01 May 2023
Jour. Geol. Soc. India (2023) 99 (5): 688–696.
... . In: Shit P.K. , Bera B. , Islam A. , Ghosh S. , Bhunia G.S. (Eds.), Drainage Basin Dynamics. Geography of the Physical Environment . Springer , Cham . doi: 10.1007/978-3-030-79634-1_14 Ghosh , S. , Bera , B. ( 2022 ) River Raidak-I Migration Dynamics Within...
FIGURES | View All (5)