Kwekwe reef prospect
A prospect the holder identified from an old geological map as a "long red oxide reef", ~4 km from both the Kwekwe partners block and Kwekwe block 2. No pegs exist yet (pegging planned 2026-07-15): the boundary shown is a nominal 1500 × 1300 m analysis window (~195 ha) around the box the holder highlighted on a GPS-app screenshot, not a claim. Three waypoints legible on that screenshot pin the reef trace itself — a ~1.1 km NE–SW line from 780734 E / 7910650 N to 779900 E / 7909989 N (UTM 35S). 87 known gold mines fall within 40 km, and 54 within 25 km — the richest local calibration set of any block in this study. This is a where-to-walk assessment on free satellite data, not a claim that gold is present.
One honest caution: current Sentinel-2 shows no elevated red-oxide staining along the mapped reef — the trace reads at the 13th percentile in ferric ratio, on fully exposed ground at 0% cloud. That does not refute the old map (the district's 54 known mines carry no ferric signal either, +0.07σ; laterite and farmed soil swamp it, and the ground may simply be cultivated over), but the satellite cannot confirm the reef as a surface red-oxide feature. The terrain arm is what backs this ground: 79th percentile against the strongest terrain model in the set (LOO AUC 0.937 on 54 mines).
The best-ground spots (UTM 35S). Spots 1–3 are the SW terminus cluster (purple); spots 5 and 6 sit on the reef trace itself (red); spot 4 is the northern control point (grey):
The reef trace, sampled
The three legible waypoints from the holder's screenshot, densified to 50 m spacing (24 samples over 1065 m) and read from the 10 m fused P(gold) grid:
| Along the reef (NE → SW) | P(gold) | Percentile vs window |
|---|---|---|
| NE waypoint 780734 E / 7910650 N | 0.256 | 50th |
| mid waypoint 780348 E / 7910324 N | 0.288 | 61st |
| SW waypoint 779900 E / 7909989 N | 0.320 | 71st |
| hottest point on the line, 779948 E / 7910025 N | 0.470 | — |
The gradient is monotonic: whatever the model is reading strengthens toward the SW end and continues just past it into the spots 1–3 cluster. The ferric ratio along the same line has median 1.407 — the 13th percentile of the window.
The five checks behind that
Each is scored over the window against the ground immediately around it.
| Check | This window | What it means |
|---|---|---|
| Terrain match | 79th percentile | scored against the terrain signature of 54 known gold mines within 25 km — the largest and most skilful local terrain ensemble in the set (LOO AUC 0.937, spatial CV at 8 km holdout 0.872) |
| Red-oxide (ferric) | 33rd percentile (13th on the reef trace) | below background on fully bare ground (S2 2025-09-27, 0% cloud); the mine calibration shows ferric is uninformative in this district anyway (54 mines at +0.07 sigma separability — laterite and farmed red soil dominate) |
| Structure / lineaments | 51st percentile | background; dominant trend 120–135 degrees; farmed flat terrain caveat applies |
| ASTER alteration (SWIR) | Al-OH 49th, carbonate/Mg-OH 49th percentile | archive day scene 2004-07-30 at 0% cloud; flat, and the 54 local mines carry no alteration signal beyond chance (Al-OH −0.04 sigma) — consistent with the sub-pixel-selvage finding across this district |
| Regional P(gold) | 0.228 whole-window (40th percentile); SW cluster 0.55–0.59 | background-level overall, with the SW reef terminus as the sole above-average ground |
Compared to your other blocks
Same estimate, run over each block:
| Block | P(gold) median | Percentile vs local background |
|---|---|---|
| Belingwe-West | 0.394 | n/a |
| Silobela site 2 (window) | 0.358 | 71st |
| Silobela site 1 (window) | 0.331 | 63rd |
| Zvishavane | 0.282 | 67th |
| Kwekwe block 3 | 0.285 | 36th |
| Kwekwe block 2 | 0.254 | 45th |
| Kwekwe reef prospect (this), whole window | 0.228 | 40th |
| Kwekwe reef prospect (this), SW cluster | 0.55–0.59 | n/a |
| Kwekwe block 1 | 0.129 | 8th |
Whole-window this is background ground, at the bottom of the Kwekwe set apart from block 1. What distinguishes it is that the above-average patch is not an arbitrary corner: it coincides with, and extends, the SW end of an independently mapped reef. An old-map structure and a satellite model agreeing on the same 300 m is a better reason to walk than either alone.
Data used
- Red-oxide (ferric): Sentinel-2, scene 2025-09-27, 10 m pixels, 0% cloud cover, 0% vegetated within the window
- Hydrothermal alteration: ASTER SWIR band ratios (Al-OH b5/b6, carbonate/Mg-OH (b6+b9)/(b7+b8)), 30 m, archive scene 2004-07-30 at 0% cloud (ASTER's SWIR died April 2008; only pre-2008 archive scenes carry usable SWIR)
- Structure and terrain: Copernicus GLO-30 elevation, 30 m pixels
- Regional P(gold) estimate: AlphaEarth surface data, 10 m pixels (native); 80 m embedding-limited grid also computed
- Reef trace: three waypoints read off the holder's GPS-app screenshot (UTM 35S); the analysis window is nominal and should be re-run against the real pegs once they exist
The single most useful next step is ground truth from the SW terminus arc, 779948 E / 7910025 N → 780022 E / 7909903 N → 780442 E / 7909833 N (UTM 35S): a handheld pXRF reading on outcrop or soil, or pan-and-grab sampling, on that one ~300 m traverse. It tests the old map's reef and the model's hottest ground in a single visit — and if the reef is real but cultivated over, that is where it should still be findable at surface.