You asked about the relationship between the Trieste pegmatite outcrops and the surveyed Geomagnetic Field Strength Anomaly
Some observations . . .
1) the sampling to date covers about 10% of the Trieste tenements.
2) while the pegs in the photos are impressive, they don't appear to be significant in elevation maps or in regular resolution satellite imagery. Sample C00428735 (53.2829 -72.2162) was taken at a high point (635m) but no spod was reported.
In the area bounded by rock sample locations the elevation varies by only 155m .
3) all reported rock sample locations are plotted, those with reported spod have a halo indicating the vis. estimated spod percent
4) there appears to be a relationship between mag.anomaly and vis.spod hits, where vis.spod seems to favour low/mid range values.
5) the pattern of rock samples is not regular, nor is it random. Many areas, within easy reach, have few samples, or none at all.
A table of rock samples with more than 15% spod is listed below.
GLTAH
|
|
| LAT | LON | Sample Number | Sample Name | Easting | Northing | Type | Spod Vis. Estm. % |
|---|
| 1 |
| 1 | 53.2775 | -72.2493 | C00428094 | TR23AS-41 | 683395 | 5906668 | Boulder | 25 |
|---|
| 2 |
| 2 | 53.2776 | -72.2493 | C00428095 | TR23AS-41 | 683393 | 5906678 | Boulder | 25 |
|---|
| 3 |
| 3 | 53.2771 | -72.2472 | C00428097 | TR23AS-43 | 683534 | 5906634 | Boulder | 25 |
|---|
| 4 |
| 4 | 53.2725 | -72.2541 | C00428065 | TR23AS-15 | 683096 | 5906098 | Outcrop | 15 |
|---|
| 5 |
| 5 | 53.2724 | -72.2541 | C00428066 | TR23AS-15 | 683095 | 5906086 | Outcrop | 15 |
|---|
| 6 |
| 6 | 53.2724 | -72.2541 | C00428067 | TR23AS-15 | 683097 | 5906087 | Outcrop | 15 |
|---|
| 7 |
| 7 | 53.2724 | -72.2527 | C00428068 | TR23AS-15 | 683189 | 5906096 | Outcrop | 15 |
|---|
| 8 |
| 8 | 53.2716 | -72.2399 | C00428069 | TR23AS-17 | 684050 | 5906034 | Outcrop | 15 |
|---|
| 9 |
| 9 | 53.2756 | -72.2528 | C00428090 | TR23AS-35 | 683167 | 5906449 | Boulder | 15 |
|---|
| 10 |
| 10 | 53.2748 | -72.2523 | C00428091 | TR23AS-40 | 683204 | 5906359 | Boulder | 15 |
|---|
| 11 |
| 11 | 53.2749 | -72.2522 | C00428092 | TR23AS-40 | 683215 | 5906375 | Boulder | 15 |
|---|
| 12 |
| 12 | 53.2779 | -72.2487 | C00428096 | TR23AS-42 | 683431 | 5906722 | Boulder | 15 |
|---|
| 13 |
| 13 | 53.2763 | -72.2485 | C00428098 | TR23AS-44 | 683456 | 5906540 | Boulder | 15 |
|---|
| 14 |
| 14 | 53.2730 | -72.2352 | C00428612 | TR23PS-006 | 684357 | 5906204 | Boulder | 15 |
|---|
| 15 |
| 15 | 53.2744 | -72.2321 | C00428614 | TR23PS-009 | 684553 | 5906367 | Outcrop | 15 |
|---|
| 16 |
| 16 | 53.2742 | -72.2332 | C00428617 | TR23PS-012 | 684480 | 5906343 | Outcrop | 15 |
|---|
| 17 |
| 17 | 53.2784 | -72.2381 | C00428630 | TR23PS-028 | 684139 | 5906803 | Outcrop | 15 |
|---|
| 18 |
| 18 | 53.2783 | -72.2388 | C00428631 | TR23PS-028 | 684092 | 5906791 | Outcrop | 15 |
|---|
| 19 |
| 19 | 53.2783 | -72.2409 | C00428632 | TR23PS-029 | 683950 | 5906780 | Outcrop | 15 |
|---|
| 20 |
| 20 | 53.2783 | -72.2429 | C00428633 | TR23PS-030 | 683817 | 5906780 | Outcrop | 15 |
|---|
| 21 |
| 21 | 53.2645 | -72.2655 | C00428673 | TR23LV-015 | 682370 | 5905186 | Boulder | 15 |
|---|
| 22 |
| 22 | 53.2715 | -72.2199 | C00428707 | TR23JW-009 | 685381 | 5906075 | Outcrop | 15 |
|---|
| 23 |
| 23 | 53.2714 | -72.2208 | C00428708 | TR23JW-009 | 685321 | 5906071 | Outcrop | 15 |
|---|
| 24 |
| 24 | 53.2714 | -72.2212 | C00428709 | TR23JW-009 | 685292 | 5906060 | Outcrop | 15 |
|---|
(20min delay)