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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_091525.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 ๐๐ from WSM reg_SO - (0, 1) Regime of ๐๐ azi_SO_010 degree (0, 180)* Interpolated azimuth of ๐๐ measured between 0-10 km azi_SO_1020 degree (0, 180)* Interpolated azimuth of ๐๐ measured between 10-20 km azi_SO_2030 degree (0, 180)* Interpolated azimuth of ๐๐ measured between 20-30 km azi_SO_3040 degree (0, 180)* Interpolated azimuth of ๐๐ measured between 30-40 km azi_SO_nofm degree (0, 180)* Interpolated azimuth of ๐๐ measured from focal mechanism azi_SO_fm degree (0, 180)* Interpolated azimuth of ๐๐ measured from other techniques azi_SL degree (0, 180)* Interpolated azimuth of ๐๐ฟ reg_SL - (0, 1) Regime of ๐๐ฟ sp1_SL Pa - Magnitude of principal stress 1 for ๐๐ฟ sp2_SL Pa - Magnitude of principal stress 2 for ๐๐ฟ azi_SM degree (0, 180)* Interpolated azimuth of feature ๐๐ reg_SM - (0, 1) Regime of ๐๐ sp1_SM Pa - Magnitude of principal stress 1 for ๐๐ sp2_SM Pa - Magnitude of principal stress 2 for ๐๐ azi_ST degree (0, 180)* Interpolated azimuth of feature ๐๐ reg_ST - (0, 1) Regime of ๐๐ sp1_ST Pa - Magnitude of principal stress 1 for ๐๐ sp2_ST Pa - Magnitude of principal stress 2 for ๐๐ azi_SB degree (0, 180)* Interpolated azimuth of feature ๐๐ต delta_SO_F degree (0, 90) ฮ๐๐โ๐น delta_SL_F degree (0, 90) ฮ๐๐ฟโ๐น delta_SM_F degree (0, 90) ฮ๐๐โ๐น delta_ST_F degree (0, 90) ฮ๐๐โ๐น delta_SB_F degree (0, 90) ฮ๐๐ตโ๐น delta_SO_R1 degree (0, 90) ฮ๐๐โ๐ 1 :1' order river delta_SL_R1 degree (0, 90) ฮ๐๐ฟโ๐ 1 delta_SM_R1 degree (0, 90) ฮ๐๐โ๐ 1 delta_ST_R1 degree (0, 90) ฮ๐๐โ๐ 1 delta_SB_R1 degree (0, 90) ฮ๐๐ตโ๐ 1 delta_F_R1 degree (0, 90) ฮ๐นโ๐ 1 delta_SO_R2 degree (0, 90) ฮ๐๐โ๐ 2 :2' order river delta_SL_R2 degree (0, 90) ฮ๐๐ฟโ๐ 2 delta_SM_R2 degree (0, 90) ฮ๐๐โ๐ 2 delta_ST_R2 degree (0, 90) ฮ๐๐โ๐ 2 delta_SB_R2 degree (0, 90) ฮ๐๐ตโ๐ 2 delta_F_R2 degree (0, 90) ฮ๐นโ๐ 2 delta_SO_R3 degree (0, 90) ฮ๐๐โ๐ 3 :3' order river delta_SL_R3 degree (0, 90) ฮ๐๐ฟโ๐ 3 delta_SM_R3 degree (0, 90) ฮ๐๐โ๐ 3 delta_ST_R3 degree (0, 90) ฮ๐๐โ๐ 3 delta_SB_R3 degree (0, 90) ฮ๐๐ตโ๐ 3 delta_F_R3 degree (0, 90) ฮ๐นโ๐ 3 delta_SO_R4 degree (0, 90) ฮ๐๐โ๐ 4 :4' order river delta_SL_R4 degree (0, 90) ฮ๐๐ฟโ๐ 4 delta_SM_R4 degree (0, 90) ฮ๐๐โ๐ 4 delta_ST_R4 degree (0, 90) ฮ๐๐โ๐ 4 delta_SB_R4 degree (0, 90) ฮ๐๐ตโ๐ 4 delta_F_R4 degree (0, 90) ฮ๐นโ๐ 4 delta_SO_R5 degree (0, 90) ฮ๐๐โ๐ 5 :5' order river delta_SL_R5 degree (0, 90) ฮ๐๐ฟโ๐ 5 delta_SM_R5 degree (0, 90) ฮ๐๐โ๐ 5 delta_ST_R5 degree (0, 90) ฮ๐๐โ๐ 5 delta_SB_R5 degree (0, 90) ฮ๐๐ตโ๐ 5 delta_F_R5 degree (0, 90) ฮ๐นโ๐ 5 delta_SO_R>1 degree (0, 90) ฮ๐๐โ๐ >1 :>1' order river delta_SL_R>1 degree (0, 90) ฮ๐๐ฟโ๐ >1 delta_SM_R>1 degree (0, 90) ฮ๐๐โ๐ >1 delta_ST_R>1 degree (0, 90) ฮ๐๐โ๐ >1 delta_SB_R>1 degree (0, 90) ฮ๐๐ตโ๐ >1 delta_F_R>1 degree (0, 90) ฮ๐นโ๐ >1 delta_SO_Z degree (0, 90) ฮ๐๐โ๐ delta_SL_Z degree (0, 90) ฮ๐๐ฟโ๐ delta_SM_Z degree (0, 90) ฮ๐๐โ๐ delta_ST_Z degree (0, 90) ฮ๐๐โ๐ delta_SB_Z degree (0, 90) ฮ๐๐ตโ๐ delta_F_Z degree (0, 90) ฮ๐นโ๐ delta_Z_R1 degree (0, 90) ฮ๐โ๐ 1 :1' order river delta_Z_R2 degree (0, 90) ฮ๐โ๐ 2 :2' order river delta_Z_R3 degree (0, 90) ฮ๐โ๐ 3 :3' order river delta_Z_R4 degree (0, 90) ฮ๐โ๐ 4 :4' order river delta_Z_R5 degree (0, 90) ฮ๐โ๐ 5 :5' order river delta_Z_R>1 degree (0, 90) ฮ๐โ๐ >1 :>1' order river *The range is not (0,360) because we only consider azimuth not directionmore » « less
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