Structural Overview and Morphotectonic Evolution of a Strike-Slip Fault in the Zone of North Almora Thrust, Central Kumaun Himalaya, India

Table 2

Sinuosity parameters calculated for various segments from Seraghat to Seri (see Figure 7(a)).

Sector/bend	CL	VL	AL	CI	VI	SSI	HSI (%)	TSI (%)
A-B	1033.33	1000	966.67	1.07	1.03	1.03	50	50
B-C	1200	1116.67	1066.67	1.12	1.05	1.07	62	38
C-D	1066.67	666.67	600	1.78	1.11	1.60	86	14
D-E	2000	1766.67	1666.67	1.20	1.06	1.13	70	30
E-F	1266.67	1100	1000	1.27	1.10	1.15	63	37
F-G	1266.67	1066.67	933.33	1.36	1.14	1.19	60	40
G-H	1266.67	1166.67	1066.67	1.19	1.09	1.09	50	50
H-I	1866.67	1800	1733.33	1.08	1.04	1.04	50	50
I-J	1800	1733.33	1666.67	1.08	1.04	1.04	50	50
J-K	2533.33	2466.67	2400	1.06	1.03	1.03	50	50
K-L	2133	1800	1733.33	1.23	1.04	1.19	83	17