
Polymetallic Deposits: When One Project Carries Multiple Metals
October 7, 2026
Government Grants for Copper Juniors: What They Really Mean for Investors
October 7, 2026
What the ground reveals before drilling begins
In commodity exploration, timing errors cost money in both directions. A drilling program launched without enough preliminary work burns capital on targets that haven’t been screened. Wait too long and a competitor stakes the same ground. Soil geochemistry sits between those two decisions: a method used to narrow down geological targets before a single drill hole goes in. A current project in southern Africa shows how this plays out in practice, and what it means for investors sizing up junior explorers.
One company active in eastern Botswana — Kavango Resources, listed on the London Stock Exchange — has used systematic soil sampling to identify two geochemical anomalies, each several kilometers wide. Both follow amphibolite host rocks, a geological setting already linked to nickel sulfide occurrences in the area. Before any drilling, the geochemistry produces a spatial pattern that roughly outlines where mineralized material might sit.
Nickel, copper, and scarce exploration capital
Nickel and copper appear on government critical minerals lists — raw materials treated as essential for electric vehicles and grid-scale energy storage. That designation has pulled substantially more early-stage investment into exploration projects than was typical before the energy transition became a political priority.
For junior explorers, this means easier access to equity financing, but also pressure to stretch limited funds. A soil sampling campaign costs a fraction of a drilling program. Analyzing 500 or 1,000 soil samples across several square kilometers produces a chemical picture of the near-surface zone without putting a drill bit in the ground.
The underlying logic: metals present at depth migrate slowly upward through chemical and physical weathering, accumulating in the soil at measurable concentrations even when the source lies hundreds of meters below. These zones are called geochemical anomalies.

From sample to priority target
Geochemical data interpretation follows a clear logic. Samples are analyzed not only for the target element — nickel, say — but also for pathfinder elements that are geologically associated with it. In nickel sulfide systems these commonly include cobalt, chromium, or sulfur.
When multiple elements correlate spatially and the anomaly coincides with a known geological structure such as amphibolite, geological confidence rises. The more independent data sources point to the same location, the more credible that target becomes. Geologists call this converging lines of evidence.
| Exploration Method | Cost Level | Depth of Insight | Typical Phase |
|---|---|---|---|
| Soil Geochemistry | Low | Near-surface | Early exploration |
| Geophysics (e.g., EM, Magnetics) | Medium | Subsurface structure | Target definition |
| RC Drilling | High | Direct, point-specific | Resource delineation |
| Diamond Core Drilling | Very high | Direct, detailed | Resource definition / MRE |
What the Botswana example tells investors
When assessing exploration companies, the quality of preliminary work matters. Multi-kilometer anomalies with strongly elevated values carry more weight than small, weak spikes. An anomaly that spatially matches a known host rock is geologically more plausible than one that sits in isolation. Historical data from the same region can also indicate whether similar patterns have previously led to real deposits.
In the Kavango case, the region has a track record as a nickel producer and the anomalies follow the same rock type associated with nearby existing deposits. That doesn’t guarantee anything, but it does suggest the team is doing preliminary work before committing to expensive drilling.
Companies that run soil geochemistry and geophysics as a connected sequence before drilling generally reduce the odds of a dry hole campaign. For an investor, that says something about how management treats capital.
Anomaly is not the same as deposit
Soil geochemistry has real limits. Throughout the history of mineral exploration, geochemical anomalies have far more often failed to develop into economic deposits than succeeded. Elevated metal values in the soil can come from many sources, most of them not exploitable.
The path from anomaly to mineral resource (classified under NI 43-101 or JORC first as an Inferred Resource, then as an Indicated or Measured Resource) is long and expensive. It requires drilling programs, metallurgical testing, and economic studies. Geochemical results sit at the very start of that chain, which is worth remembering when reading company announcements.
One thing has changed: because nickel and copper now appear on supply-security lists in Europe, the United States, and elsewhere, well-documented early-stage projects attract capital market attention that would have been unusual in prior cycles. This shifts the funding environment for junior explorers, but it does not change what individual geochemical results actually mean in the ground.
Key terms
- Soil geochemistry
- The systematic sampling of soil for its chemical composition to identify clues about subsurface mineralization. A low-cost, early-stage exploration method.
- Geochemical anomaly
- A zone where one or more elements in a soil sample are statistically well above the regional background value — a possible indicator of underlying mineralization.
- Pathfinder elements
- Elements geologically associated with a target element that help locate it because they are more mobile or more readily detectable at the surface.
- Amphibolite
- A metamorphic rock that commonly acts as a host rock for nickel sulfide mineralization. In Botswana, it is associated with known Ni-Cu deposits.
- Critical minerals
- Raw materials classified by governments as essential for the energy transition, defense, and technology, with supply considered geopolitically sensitive (e.g., nickel, copper, cobalt, lithium).
- Inferred resource
- The lowest confidence category of a mineral resource under NI 43-101 or JORC. Based on limited data; must not be confused with a reserve and does not imply economic extractability.
- Junior explorer
- A small mining company in the early stages of exploration with no production of its own, raising capital through equity markets to advance geological projects.
- Converging lines of evidence
- A principle in exploration geology: when multiple independent methods (geochemistry, geophysics, geology) all point to the same target area, the credibility of that target increases.
⚠️ Important notice: This article is for informational and educational purposes only. It does not constitute investment advice, a recommendation, or a solicitation to buy or sell any security. Investments in small-cap exploration and mining companies carry a high risk, including the potential total loss of capital. Before making any investment decision, consult a registered financial advisor and conduct your own analysis. Boersen Post Team is not responsible for decisions taken based on the content published here.



