Overview

Mine Type	Underground
Stage	Construction
Commodities	Polyhalite
Mining Method	Continuous
Production Start	...
Mine Life	...
Snapshot	The Woodsmith Project is the largest known high-grade polyhalite deposit in the world. The fertiliser product – known as POLY4 – will be exported to a network of customers overseas from port facility at Teesside. The estimates remain unchanged on the basis that the full technical update and techno-economic review of the project is still to be presented to the Anglo American Board in 2025. The outcome of these studies may result in changes to the LoAP, Reserve Life and Ore Reserve and Mineral Resource estimates. Sinking activities at the two deep shafts continue to progress well. The service shaft is now c.745 metres deep, having reached the expected depth for the 2023 year. Anglo American enhancing the project’s configuration to allow a higher production capacity, a final design capacity of 13 Mtpa is subject to studies and approval.

Deposit type

• Sedimentary

Summary:

The deposit is part of the Late Permian evaporite succession on the western edge of the Zechstein Basin, which represents multiple influxes and subsequent evaporation of seawater in a topographic low with restricted connection to the Zechstein Sea. The polyhalite sits within the EZ2 Fordon Evaporite sequence, a significant basin-infilling cycle. This sequence varies between 30 and 200 m thick across the project area, thickening to the east, towards the centre of the basin.

The polyhalite appears to be formed by synsedimentary metasomatism or back-reaction of pre-existing sulphates; gypsum/anhydrite, with potassium and magnesium-enriched marine brines. The deposit is a stratiform sedimentary unit displaying significant lateral continuity. It is composed of two high grade seams: the Shelf Seam and the Basin Seam.

The Shelf Seam exists on the basin margin and thickens in the central part of the project area before pinching out to the east. It is bound by intergrown halite anhydrite-polyhalite below and anhydrite above. The Basin Seam is deeper and bound by halite; it terminates against the base of the palaeo-ramp to the east and extends out to the west under the North Sea. On a smaller scale, the deposit is modelled as a series of laterally continuous units within the Shelf Seam, potentially representing variations in the sea level and depositional environment of the Zechstein Sea at the time. Three zones of high grade polyhalite are distinguished, separated by anhydrite-dominated bands.

The Basin Seam is one of two high grade polyhalite seams within the Woodsmith deposit. It is deeper than the Shelf Seam, is bound by halite, and terminates against the base of the palaeo-ramp to the west and extends out to the east under the North Sea.

Mining Methods

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Comminution

Crushers and Mills

Processing

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Production

Personnel

Job Title	Name	Profile	Ref. Date
.......................	.......................		Mar 22, 2024
.......................	.......................		Mar 22, 2024
.......................	.......................		Mar 22, 2024
.......................	.......................		Mar 22, 2024
.......................	.......................		Mar 22, 2024
.......................	.......................		Mar 22, 2024

Total Workforce	Year
......	2020