Member Info for Yogi1

The green diamond fits the lamproite model perfectly. Natural green diamonds are extremely rare.

Their preservation requires:

• Low‑temperature ascent

• Volatile‑rich magma

• Minimal resorption

Lamproites are exceptionally good at preserving coloured diamonds — Argyle pinks, Ellendale yellows.

So the green diamond is not random. It is a lamproite‑compatible diamond.

And its dispersion fan overlaps:

• Seitaperä

• Riihivaara

• Anomaly 5

This is a huge geological signal.

Three lamproite bodies in one corridor = a real lamproite province

You now have:

1. Seitaperä

• Large lamproite blow (6.9 ha)

• Diamondiferous

• Proven mantle fertility

2. Riihivaara

• Lamproite dyke

• Fertile indicator chemistry

• Open along strike and down‑dip

3. Anomaly 5

• Lamproite breccia

• On the margin of a larger EM anomaly

• Geometry consistent with a pipe or vent

This is exactly how lamproite provinces form:

• Argyle Field → multiple lamproites

• Ellendale Field → dozens of lamproites

• Prairie Creek Field → lamproite dykes + pipes

Kuhmo now fits the same pattern.

Why it this Kuhmo district now more appealing

Because now the district has:

1. A proven diamondiferous lamproite (Seitaperä)

→ mantle fertility confirmed

2. A second lamproite with excellent chemistry (Riihivaara)

→ feeder system confirmed

3. A third lamproite with pipe‑style geometry (Anomaly 5)

→ potential economic body

4. A fancy‑colour diamond already recovered

→ high‑value upside

This combination is rare. Most lamproite fields never produce a single diamond. Kuhmo has already produced multiple diamonds, including a green one.

So does Seitaperä being lamproite make Riihivaara and Anomaly 5 more appealing?

Yes — massively.

Because it means:

You are not dealing with isolated intrusions. You are dealing with a lamproite province with proven diamond fertility.

This is exactly the scenario that precedes major discoveries.

Its worth remembering that Riihivaara is also lamproite as well as Seitapera and Anomaly 5.

Riihivaara is a fertile lamproite, not just any lamproite. The mantle signal at Riihivaara is the important bit:

• Garnets: Presence of eclogitic, diamond‑type garnets (G10‑style chemistry) → sampling of cool, high‑pressure lithospheric mantle.

• Chromites: Diamond‑type chromites (high Cr, low Ti) → compatible with diamond stability field.

• Ilmenite: Chemistry consistent with non‑destructive ascent temperatures → diamonds, if present, are less likely to have been resorbed.

So “lamproite at Riihivaara” really means “lamproite that has sampled diamond‑compatible mantle and didn’t cook it to death”. That’s a big upgrade from just “lamproite present”.

Rio Tinto rated Riihivaara far more highly than most people realise — and for reasons that are very specific to Rio’s internal diamond strategy, their lamproite expertise, and the mantle signature at Riihivaara.

It’s time KDR and its share price started moving. In my biased view the market cap should be way higher here and warrants would then get exercised. This is an exciting story that the market has not recognized yet.

Gem‑Quality Comparison: Lahtojoki vs. Argyle, Diavik, Orapa

🟥 Argyle (Australia) — Very low gem‑quality percentage

Argyle was one of the world’s largest producers by volume, but the proportion of gem‑quality diamonds was low.

Produced mostly brown, champagne, and industrial‑grade stones.

Famous for pink diamonds, but these were extremely rare relative to total output.

Overall gem‑quality ratio: low single digits to low teens (inferred from “low proportion” and industry data).

🟦 Diavik (Canada) — High gem‑quality percentage

Diavik is widely known (outside the provided sources) for producing high‑value, high‑clarity white diamonds.

Industry‑standard estimates place Diavik’s gem‑quality ratio at 50–70% (inference based on its reputation for premium stones).

🟧 Orapa (Botswana) — Moderate gem‑quality percentage

Industry‑typical values for Orapa are 20–30% gem‑quality, with the remainder industrial.

Orapa is a high‑volume mine, but not known for unusually high gem‑quality output.

🟩 Lahtojoki (Finland) — Estimated ~60% gem‑quality

Previous results indicate that Lahtojoki hosts high‑quality gem diamonds, including rare pink and coloured stones that can fetch up to 20× the price of colourless diamonds.

If Lahtojoki’s gem‑quality ratio is indeed ~60%, it would:

Exceed Orapa

Dramatically exceed Argyle

Be comparable to Diavik

Place it among the higher‑value kimberlite deposits globally

Lahtojoki’s estimated ~60% gem‑quality ratio would place it well above several major global diamond mines, especially Argyle and Orapa, and roughly comparable to or slightly below Diavik.

So what does it actually predict for Lahtojoki?

It suggests:

The mantle beneath Lahtojoki is diamond‑fertile

The kimberlite should contain both eclogitic and peridotitic diamonds

The deposit has a realistic chance of being economic

The grade will depend on dilution, eruption dynamics, and diamond preservation, not mantle fertility alone

In other words:

1% diamond in a xenolith means the mantle is excellent. The kimberlite grade depends on everything that happened afterward.

What this means for economic grade predictions

Here’s the honest, technical interpretation used by diamond geologists:

1. It raises the “geological ceiling” for diamond grade

If the mantle can produce 1% diamond in eclogite, then the maximum possible grade for the kimberlite is higher than in provinces where eclogites contain almost no diamond.

This doesn’t guarantee a high grade — it just expands the potential.

2. It increases confidence that the kimberlite sampled diamond‑rich zones

Kimberlites are chaotic. They entrain mantle material randomly. Finding a 1% diamond xenolith means:

The eruption passed through a diamond‑rich mantle domain

Diamonds were available to be picked up as xenocrysts

The kimberlite likely contains a mixed diamond population, including eclogitic stones

This is why Lahtojoki has both eclogitic and peridotitic diamonds.

3. It supports the idea that the Karelian Craton is a legitimate diamond province

Before these xenoliths were found, Finland’s diamond potential was uncertain. Afterward, the mantle model looked much more like:

Northern Russia (Grib, Lomonosov)

Northern Canada (Slave Craton)

Both are world‑class diamond regions.

4. It does not directly translate to ore grade

A kimberlite with 1% diamond would be:

10,000 carats per tonne

Economically impossible

Geologically absurd

Commercial grades are usually:

0.1–2 carats per tonne (economic)

2–10 cpt (exceptional)

>10 cpt (world‑class, extremely rare)

So the xenolith’s 1% diamond content is not a grade prediction — it’s a mantle fertility indicator.

Why 1% diamond in a xenolith is extraordinary

Most diamondiferous eclogites worldwide contain:

0.01–0.1% diamond (typical)

0.3–0.5% (rare, high)

1% (extremely rare, only a handful of occurrences globally)

So Lahtojoki’s xenoliths sit at the very top end of diamond concentration in mantle rocks.

This tells you the mantle beneath the Kaavi–Kuopio field is:

deep, cool, and stable

strongly diamond‑favourable

rich in eclogitic carbon

metasomatised by reduced, CH₄‑bearing fluids

All of these are the same conditions seen beneath Grib, Lomonosov, Udachnaya, Orapa, and Diavik.

Eclogite is the important word….. Lahtojoki has it.

A 1% diamond content which Lahtojoki has in an eclogite xenolith sounds small, but in kimberlite economics it’s a huge signal. It does not mean the Lahtojoki kimberlite itself contains 1% diamond. Instead, it tells you something far more important: the mantle source beneath Lahtojoki is capable of producing extremely diamond‑rich material. A xenolith containing ~1 wt% diamond is a geological “smoking gun” that the mantle beneath Lahtojoki is highly diamond‑fertile — but it does not predict a 1% grade in the kimberlite.

Instead, it raises the upper bound of what the mantle can produce and increases confidence in the deposit’s diamond potential.

The market will slowly start to understand what KDR have and the share price will eventually start reflecting KDRs potential. Hopefully soon

Karelian Diamond Resources has far more strings to its bow than most investors realise. Some are obvious (Lahtojoki), some are emerging (Kuhmo), and some are strategic leverage points that only become valuable when viewed as part of a portfolio.

Does the delay change the strategic attractiveness of KDR? No.

Lahtojoki remains:

• The only permitted diamond mine in the EU

• A low‑capex, short‑construction project

• A high‑margin niche producer

• In a geopolitically safe jurisdiction

• With a diamond market entering structural shortage

The delay is procedural, not geological or commercial.

How the delay affects partner‑readiness

A. No serious partner will commit before compensation is final

This is absolute. Any potential partners will probably not sign a JV or financing package until:

“All landowner compensation is final and legally binding.”

This is standard in Finland and globally.

B. The delay slows — but does not damage — partner interest

Partners don’t walk away because of a procedural delay. They simply wait. What matters to them is:

• The orebody

• The permit

• The economics

• The jurisdiction

• The long‑term diamond supply deficit

None of those are affected by the NLS review.

C. The delay pushes back the partner‑engagement window

Realistically:

• Compensation finalised → partner discussions accelerate

• Partner discussions → financing structure

• Financing → construction decision

How the delay affects KDR’s valuation

A. The market applies a “time discount” to value

Lahtojoki’s NPV doesn’t fall because of the delay — the orebody hasn’t changed — but the market applies a discount because:

• Cashflows are pushed further into the future

• Financing is delayed

• Construction start is delayed

• The company remains in a pre‑development risk category

This is why KDR trades at £1.6m (approx) market cap despite holding a fully permitted diamond mine.

B. The delay keeps KDR in the “administrative risk” bucket

Investors hate uncertainty around:

• Landowner disputes

• Compensation

• Appeals

• Procedural bottlenecks

Until compensation is finalised, KDR is still seen as a company with unresolved permitting risk, even though the mine permit itself is secure.

C. The delay prevents the market from re‑rating the asset

Once compensation is finalised, Lahtojoki moves into:

• “Financeable project”

• “JV‑ready project”

• “Construction‑ready project”

That shift alone would normally trigger a 50–150% re‑rating for a microcap explorer transitioning into a development‑stage miner.

The delay simply postpones that re‑rating.

I wonder will we get news of the compensation all sorted soon. The Lahtojoki delay is entirely due to the National Land Survey needing to re‑evaluate three compensation items that the Land Court sent back for review. Everything else — boundaries, appeals, rental payments — is already resolved. The delay does affect KDR’s valuation and partner‑readiness, but only in one specific way: it pushes back the point at which Lahtojoki becomes a financeable, de‑risked mining project. It does not reduce the underlying value of the asset, but it delays when that value can be recognised by the market or by a strategic partner.

I can see this doubling in the month of May for starters. Be interesting to watch. Just my biased opinion, but some logic behind that too.

Market makers holding this back. Should be climbing.

Actually our marked cap is less than what I said…. Think it’s £1.6