Location,Grid Coordinates,,Point,K (%),U (ppm),Th (ppm),DR (nGy/h),Heat Production,Reading Length (mins),Notes,,,,
,Northing,Easting,,,,,,,,,,,,
1,"56?59'52.3""","002?30'34.9""",1,5.37,8.81,40.11,220.27,5.63,5.00,"Pink granite of coarse (5mm) crystals, at ""coves of curran""",,,,
,,,2,5.38,6.75,46.11,223.66,5.51,,,,,,
,,,3,4.91,8.21,44.32,221.48,5.73,,,,,,
2,"56?59'44.8""","002?30'34.9""",1,4.95,9.42,49.28,241.13,6.39,,,,,,
,,,2,5.35,10.30,42.43,234.31,6.18,,,,,,
3,"56?59'45.2""","002?31'10.6""",1,5.71,9.34,50.22,252.92,6.51,,"Series of fractures, set1 50?/091? set2 82/050? set3 60?/194?. Set2 observed to terminate against set1",,,,
,,,2,5.47,11.42,44.72,247.91,6.65,,,,,,
4,"56?59'24.6""","002?31'29.4""",1,5.39,11.65,44.40,247.33,6.68,,Melmannoch,,,,
,,,2,5.46,10.35,50.31,255.71,6.76,,,,,,
,,,3,5.45,12.28,46.30,256.43,6.98,,,,,,
5,"56?59'24.6""","002?31'29.4""",1,4.45,14.34,47.12,257.06,7.48,,"Top of gentle ridge, two fracture sets set1 68?/335? set2 89?/230?",,,,
,,,2,5.07,12.57,47.41,255.85,7.10,,,,,,
6,"57?00'49.4""","002?54'37.3""",1,3.74,13.24,45.31,237.08,7.00,,Glacial Tor on ridge 600m North of Clachan Yell. Coarse grained pink granite. Granite outcrop is onion skin weatherd and rounded adges show it has been exposed a while. Photo 5288,,,,
,,,2,4.16,10.82,42.07,220.74,6.18,,,,,,
,,,3,4.26,12.06,39.68,223.69,6.35,,,,,,
7,"57?00'30.3""","002?54'47.1""",1,4.53,13.54,46.69,252.51,7.25,,Tor on North side of Clachan Yell,,,,
,,,2,3.97,13.57,43.73,237.99,7.00,,,,,,
8,"57?00'28.4""","002?54'49.0""",1,4.87,12.82,45.13,249.06,6.99,,Glacial Tor to South of Clachan Yell Summit,,,,
,,,2,4.90,11.53,45.98,244.73,6.71,,,,,,
9,"57?02'05.8""","002?53'25.1""",1,5.02,24.42,42.24,309.55,9.84,,"River Bank in Glen Tanar, granite is higly fractured and river is straight so river likely follows a faults. Possible Fualt would have strike of W-E. Measurements here might be slightly >2?",,,,
,,,2,4.83,25.49,40.89,309.76,10.00,,,,,,
10,"56?57'02.1""","002?38'04.8""",1,4.12,12.17,37.37,216.22,6.20,,"Centre of Tor at Cairn of Finglenny. Granite here is coarse grained crystals with megacrysts upto 3-5cm. Pink coloured feldspar. Well weathered with round edges. Outcrop is highly jointed, joints are subvertical with general strike of WSW-ENE. Joint spacing approx. 50cm. Possible underestimate in readings due to closely spaced joints filled with organic material.",,,,
,,,2,4.36,9.64,40.91,213.78,5.81,,,,,,
,,,3,4.58,8.42,44.40,218.42,5.75,,,,,,
11,"56?57'01.9""","002?38'04.5""",1,4.84,8.69,41.10,215.17,5.62,,South side of Cairn of Finglenny,,,,
,,,2,4.38,9.54,41.99,216.13,5.86,,,,,,
12,"56?57'02.3""","002?38'06.2""",1,4.75,10.40,45.93,235.64,6.40,,Good exposure 10m west of cairn of Finglenny,,,,
,,,2,4.58,11.80,45.63,240.64,6.73,,,,,,
13,"56?57'31.4""","002?39'06.0""",1,4.24,9.32,39.62,207.16,5.62,,"Cairn of Edendocher. Coarse grained weathered pink granite. Heavily jointed at spacing approx. 50cm. Joints subvertical striking WSW-ENE. Some perpendicular joint laddering (NNW-SSE), this perpendicular set terminated againts any intersection with the WSW-ENE joint set. Joints apertures are 5-10cm filled with oranic matter, the one ok reading site used for 8,9 may still be underestimated. There are no other suitable locations for readings on this outcrop. Photo 5291 of points 8,9, photo in direction of ENE anc can be seen main joints set with perepndicular laddering. ",,,,
,,,2,4.11,8.67,38.68,199.39,5.37,,,,,,
14,"56?58'06.7""","002?38'15.9""",1,4.04,23.56,119.93,485.58,14.97,,On outcrop SE of Clachnaben. Third measurement (16) is next to other two just to check extraordinarily high results.,,,,
,,,2,3.84,23.05,124.57,491.66,15.14,,,,,,
,,,3,4.39,16.58,98.00,395.92,11.64,,,,,,
15,"56?58'06.3""","002?38'16.1""",1,4.32,8.86,40.84,208.60,5.60,,Same outcrop as before but on SW corner to check previous results. Outcrop joints are subvertical and orientated W-E/WSW-ENE with perpencicular laddering. Also contains horizontal joints.,,,,
,,,2,4.41,10.67,36.13,208.32,5.75,,,,,,
16,"56?58'06.7""","002?38'15.9""",1,4.84,11.49,39.06,225.89,6.21,,"2m from 10,11 to cbheck how isoltated U, Th enrichment is",,,,
,,,2,4.81,11.48,40.69,229.59,6.32,,,,,,
17,"56?58'05.1""","002?38'03.0""",1,4.91,13.99,44.68,255.07,7.26,,Clachnaben. Joints are subvertical WNW-ESE. Regular onion skin weathering. ,,,,
,,,2,4.84,13.50,46.37,252.88,7.25,,,,,,
18,"56?58'04.8""","002?38'03.2""",1,4.96,8.99,44.45,226.66,5.94,,"Two intersecting sets of big fractures, no sense of slip but they cross eac other with no termination indicating mode 2 deformation. Set1 86?/118? set2 80?/019? photo 5292- frac 1 in right of photo frac 2 in left of photo",,,,
,,,2,4.75,9.44,45.89,230.16,6.14,,,,,,
19,"56?58'22.7""","002?37'26.1""",1,6.89,7.85,59.93,284.18,6.91,,Outcrop in the slack of Dye. Cross-cutting fractures set1 80?/265? set2 80?/171? (sinstral sense of shear) set3 82?/218? likely mode 1,,,,
,,,2,6.04,8.76,43.98,238.35,5.95,,,,,,
,,,3,5.80,9.50,40.58,230.96,5.88,,,,,,