Locality · Cumbria

The Caldbeck Fells

A small area of northern Lakeland that produced some of the most distinctive lead secondaries in Britain, campylite above all.

Region CumbriaBest known for Campylite, pyromorphite

The Caldbeck Fells hold a remarkable density of old workings in a compact area of northern Cumbria, mined for lead and copper from the 1700s. Dry Gill produced campylite, the barrel-shaped arsenian mimetite that is the district's signature. Roughton Gill yielded pyromorphite, linarite and leadhillite. Specimens are small — typically under 5 cm.

In short

  • The Caldbeck Fells are a compact area on the northern edge of the Lake District with a remarkable density of old workings.
  • Campylite — the barrel-shaped, orange-brown arsenian variety of mimetite — is the signature material, classically from Dry Gill.
  • Roughton Gill produced pyromorphite, linarite, leadhillite and plumbogummite.
  • Nearly all material is old; the workings are long disused and largely within protected landscape.
  • Specimens are small. This is thumbnail and miniature country, not cabinet.
The principal Caldbeck workings
WorkingSignature speciesCharacter
Dry GillCampyliteBarrel-shaped orange-brown crystals on gossan
Roughton GillPyromorphite, linarite, leadhilliteThe most species-diverse of the group
Red GillLinarite, caledoniteDeep blue secondaries
Brandy GillWolframite, arsenopyritePrimary rather than secondary

Campylite, and why it looks like nothing else

Campylite is not a separate species — it is the arsenian variety of mimetite — but it is visually distinctive enough that the old name has survived in the trade. The crystals are barrel-shaped rather than prismatic, typically warm orange to brown, and sit on a dark limonitic gossan that sets them off perfectly.

Dry Gill is the classic source, and a good Dry Gill campylite is one of the most recognisable British specimens there is.

Small, old, and finite

Two things constrain Caldbeck material. It is small — these are thumbnail and miniature specimens, and a genuinely large cabinet piece is exceptional. And it is old, because the workings have been disused for a very long time and the fells are within a protected landscape where collecting is not a matter of turning up with a hammer.

What circulates is therefore largely nineteenth and twentieth century collection material, which puts a premium on labels and documented provenance.

Roughton Gill's range

Roughton Gill is the more species-diverse of the two famous workings, producing pyromorphite in good greens, linarite in a deep blue that photographs badly and looks superb in hand, leadhillite, and plumbogummite — sometimes as pale blue coatings pseudomorphing pyromorphite, which is a Caldbeck speciality.

Questions

What is campylite?
The arsenian variety of mimetite, distinguished by barrel-shaped orange-brown crystals. Classically from Dry Gill in the Caldbeck Fells.
Can you still collect in the Caldbeck Fells?
The workings are long disused and lie within a protected landscape. Nearly all material on the market is old collection material rather than recently collected.
How large are Caldbeck specimens?
Small. Thumbnails and miniatures are the norm and a large cabinet piece is exceptional.