62 MILLION
YEARS OF
FILTRATION,
extracted daily.

February 2026 production output

0
Diatomaceous Earth·SiO₂ ≥ 85%·Filtration Grade·Food-Grade Certified·62 Million Years·ISO 13320 Tested·Calcined & Natural Grades·48.7M Ton Reserve·Diatomaceous Earth·SiO₂ ≥ 85%·Filtration Grade·Food-Grade Certified·62 Million Years·ISO 13320 Tested·Calcined & Natural Grades·48.7M Ton Reserve·

Today's Output

DE-F10
91.2%
0.4%
212
DE-M25
88.7%
0.6%
178
DE-C40
94.1%
0.2%
134
DE-AG
85.3%
0.8%
203
DE-P08
95.8%
0.1%
88
DE-I15
87.4%
0.5%
32
8%
22%
38%
24%
8%
SiO₂ Purity
91.2%
Fe₂O₃
0.8%
Al₂O₃
4.1%
CaO
0.3%

Deposit Cross-Section

Topsoil & Overburden
Transitional Clay
DE Horizon A — PrimaryDE Zone
DE Horizon B — SecondaryDE Zone
Volcanic Ash Interlayer
Basal DE Horizon C
2,340
48.7
0.8
14.2
7
57+
Geological drill core samples showing diatomite sediment layers in core boxes
DE Horizon A — 11.4m to 19.2m depth

62 Million Years,
layer by layer.

Modern OverburdenNon-DE
Late Miocene ClayClay
Miocene DE AccumulationDE Grade B
Eocene–Oligocene PeakDE Grade A ★
Early Eocene Lake FormationDE Grade C
Basement BasaltBedrock
Electron microscope image of diatom frustules showing intricate silica skeleton structure
Cyclotella meneghiniana — dominant species, Grade A horizon
62M
10–80μm
~90%
1M+
PALEOLAKE SEAM — EOCENE EXTENT● Active extraction zones

Full d10/d50/d90 particle size data for DE-F10, DE-M25, DE-C40, DE-AG, DE-P08, and DE-I15 grades. ISO 13320 laser diffraction method.

The Complete Deposit Analysis.

78 pages. Six grades. One lakebed. Everything a procurement engineer needs to justify a supplier switch — grade consistency data, reserve life, processing methodology, and certification documentation.

PDF
Full XRF Oxide Analysis
Particle Size Distribution — All Grades
Stratigraphic Core Log BH-44
Reserve Estimation Report
Food-Grade & SDS Certificates
Processing & Calcination Data

Updated February 2026. Includes XRF batch data from Q4 2025 and Q1 2026 production runs. Suitable for vendor qualification documentation.

Download Full Deposit Analysis

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