Unraveling the Connection between Subsurface Stress and Geomorphic Features: Dataset

This repository stores data using for the manuscript: Unraveling the Connection between Subsurface Stress and Geomorphic Features

The data file used in this study is 'Input_stress_fault_river_BK_022125.csv'.

The code used to reproduce all figures in the manuscript is 'Kuhasubpasin_et_al_2025.ipynb'

The file contain these following data:

Column
unit
range
description

lat
degree
(-90, 90)
Latitude

lon
degree
(-180, 180)
Longitude

azi_R
degree
(0, 180)*
Interpolated azimuth of river network (interpolate without considering river order)

azi_r1
degree
(0, 180)*
Interpolated azimuth of 1'-order river

azi_r2
degree
(0, 180)*
Interpolated azimuth of 2'-order river

azi_r3
degree
(0, 180)*
Interpolated azimuth of 3'-order river

azi_r4
degree
(0, 180)*
Interpolated azimuth of 4'-order river

azi_r5
degree
(0, 180)*
Interpolated azimuth of 5'-order river

Drainage_area
cell
-
Drainage area

river_order
order
(1, 7)
Majority of the order river in grid cell

elev
km
(0, 5.1375)
Elevation

TcstDens
g/cm^3
(2.7439,2.962)
Average crustal density from CRUST 1.0

TcstThk
km
(5.0731 73.517)
Total crustal thickness from CRUST 1.0

crust_type

Crustal type from ECM1

Te
km
(1,200)
Effective elastic thickness

MI
-
(-1,1)
Mantle influence index

azi_Z
degree
(0, 180)*
Topographic aspect

azi_F
degree
(0, 180)*
Interpolated azimuth of faults

reg_F
-
(0, 1)
Regime of F

azi_SO
degree
(0, 180)*
Interpolated azimuth of feature 𝜎𝑂 from WSM

reg_SO
-
(0, 1)
Regime of 𝜎𝑂

azi_SO_010
degree
(0, 180)*
Interpolated azimuth of 𝜎𝑂 measured between 0-10 km

azi_SO_1020
degree
(0, 180)*
Interpolated azimuth of 𝜎𝑂 measured between 10-20 km

azi_SO_2030
degree
(0, 180)*
Interpolated azimuth of 𝜎𝑂 measured between 20-30 km

azi_SO_3040
degree
(0, 180)*
Interpolated azimuth of 𝜎𝑂 measured between 30-40 km

azi_SO_nofm
degree
(0, 180)*
Interpolated azimuth of 𝜎𝑂 measured from focal mechanism

azi_SO_fm
degree
(0, 180)*
Interpolated azimuth of 𝜎𝑂 measured from other techniques

azi_SL
degree
(0, 180)*
Interpolated azimuth of 𝜎𝐿

reg_SL
-
(0, 1)
Regime of 𝜎𝐿

sp1_SL
Pa
-
Magnitude of principal stress 1 for 𝜎𝐿

sp2_SL
Pa
-
Magnitude of principal stress 2 for 𝜎𝐿

azi_SM
degree
(0, 180)*
Interpolated azimuth of feature 𝜎𝑀

reg_SM
-
(0, 1)
Regime of 𝜎𝑀

sp1_SM
Pa
-
Magnitude of principal stress 1 for 𝜎𝑀

sp2_SM
Pa
-
Magnitude of principal stress 2 for 𝜎𝑀

azi_ST
degree
(0, 180)*
Interpolated azimuth of feature 𝜎𝑇

reg_ST
-
(0, 1)
Regime of 𝜎𝑇

sp1_ST
Pa
-
Magnitude of principal stress 1 for 𝜎𝑇

sp2_ST
Pa
-
Magnitude of principal stress 2 for 𝜎𝑇

azi_SB
degree
(0, 180)*
Interpolated azimuth of feature 𝜎𝐵

delta_SO_F
degree
(0, 90)
Δ𝜎𝑂−𝐹

delta_SL_F
degree
(0, 90)
Δ𝜎𝐿−𝐹

delta_SM_F
degree
(0, 90)
Δ𝜎𝑀−𝐹

delta_ST_F
degree
(0, 90)
Δ𝜎𝑇−𝐹

delta_SB_F
degree
(0, 90)
Δ𝜎𝐵−𝐹

delta_SO_R1
degree
(0, 90)
Δ𝜎𝑂−𝑅1 :1' order river

delta_SL_R1
degree
(0, 90)
Δ𝜎𝐿−𝑅1

delta_SM_R1
degree
(0, 90)
Δ𝜎𝑀−𝑅1

delta_ST_R1
degree
(0, 90)
Δ𝜎𝑇−𝑅1

delta_SB_R1
degree
(0, 90)
Δ𝜎𝐵−𝑅1

delta_F_R1
degree
(0, 90)
Δ𝐹−𝑅1

delta_SO_R2
degree
(0, 90)
Δ𝜎𝑂−𝑅2 :2' order river

delta_SL_R2
degree
(0, 90)
Δ𝜎𝐿−𝑅2

delta_SM_R2
degree
(0, 90)
Δ𝜎𝑀−𝑅2

delta_ST_R2
degree
(0, 90)
Δ𝜎𝑇−𝑅2

delta_SB_R2
degree
(0, 90)
Δ𝜎𝐵−𝑅2

delta_F_R2
degree
(0, 90)
Δ𝐹−𝑅2

delta_SO_R3
degree
(0, 90)
Δ𝜎𝑂−𝑅3 :3' order river

delta_SL_R3
degree
(0, 90)
Δ𝜎𝐿−𝑅3

delta_SM_R3
degree
(0, 90)
Δ𝜎𝑀−𝑅3

delta_ST_R3
degree
(0, 90)
Δ𝜎𝑇−𝑅3

delta_SB_R3
degree
(0, 90)
Δ𝜎𝐵−𝑅3

delta_F_R3
degree
(0, 90)
Δ𝐹−𝑅3

delta_SO_R4
degree
(0, 90)
Δ𝜎𝑂−𝑅4 :4' order river

delta_SL_R4
degree
(0, 90)
Δ𝜎𝐿−𝑅4

delta_SM_R4
degree
(0, 90)
Δ𝜎𝑀−𝑅4

delta_ST_R4
degree
(0, 90)
Δ𝜎𝑇−𝑅4

delta_SB_R4
degree
(0, 90)
Δ𝜎𝐵−𝑅4

delta_F_R4
degree
(0, 90)
Δ𝐹−𝑅4

delta_SO_R5
degree
(0, 90)
Δ𝜎𝑂−𝑅5 :5' order river

delta_SL_R5
degree
(0, 90)
Δ𝜎𝐿−𝑅5

delta_SM_R5
degree
(0, 90)
Δ𝜎𝑀−𝑅5

delta_ST_R5
degree
(0, 90)
Δ𝜎𝑇−𝑅5

delta_SB_R5
degree
(0, 90)
Δ𝜎𝐵−𝑅5

delta_F_R5
degree
(0, 90)
Δ𝐹−𝑅5

delta_SO_R>1
degree
(0, 90)
Δ𝜎𝑂−𝑅>1 :>1' order river

delta_SL_R>1
degree
(0, 90)
Δ𝜎𝐿−𝑅>1

delta_SM_R>1
degree
(0, 90)
Δ𝜎𝑀−𝑅>1

delta_ST_R>1
degree
(0, 90)
Δ𝜎𝑇−𝑅>1

delta_SB_R>1
degree
(0, 90)
Δ𝜎𝐵−𝑅>1

delta_F_R>1
degree
(0, 90)
Δ𝐹−𝑅>1

delta_SO_Z
degree
(0, 90)
Δ𝜎𝑂−𝑍

delta_SL_Z
degree
(0, 90)
Δ𝜎𝐿−𝑍

delta_SM_Z
degree
(0, 90)
Δ𝜎𝑀−𝑍

delta_ST_Z
degree
(0, 90)
Δ𝜎𝑇−𝑍

delta_SB_Z
degree
(0, 90)
Δ𝜎𝐵−𝑍

delta_F_Z
degree
(0, 90)
Δ𝐹−𝑍

*The range is not (0,360) because we only consider azimuth not direction