Next generation ERW sensing.
Step 1
Rock dust reacts with natural carbonic acid in agricultural fields
Step 2
The stored CO2 flows through soil and sensor as carbonate alkalinity
Step 3
Sensor measures cumulative carbonate alkalinity in-situ and uploads data
Introducing Everest
Accurate, affordable & scalable measurement for Enhanced Rock Weathering.
Our Technology
Effortless and Accurate Alkalinity Measurement
Win Buyer Trust
Trace every single carbon credit to its origin using our comprehensive measurement history
Lower Uncertainty
Get a crystal clear liquid-phase signal through time-integrated alkalinity measurement
Reduce Cost
Leverage our automatic sensor to eliminate the cost of manual sampling
Enhanced Rock Weathering
How ERW Removes Carbon
Natural rock weathering has regulated the Earth’s temperature throughout geological history and maintained the habitability of our planet. Enhanced Rock Weathering (ERW) accelerates this natural carbon removal mechanism by strategically deploying finely ground rocks in conditions that accelerate weathering.
Step 1
Farmers spread ground rocks on their fields
Abundant alkaline rocks like basalt are repurposed from unused fines or processed to fine powders using common mining infrastructure. The small particle size increases the relative surface area of the rocks, thereby “enhancing” the speed of their weathering by many orders of magnitude. The rock powder is then transported to agricultural fields and spread by farmers using existing equipment.
CO2 concentrations in biologically active soils can be orders of magnitude higher than in the atmosphere, making them the perfect environment for rock weathering as the higher CO2 concentrations speed up the process, while the consumption of excess acidity acid balances pH.
Step 2
Alkaline rocks neutralize carbonic acid in soils
Alkaline minerals react with carbonic acid (H2CO3), which naturally forms when CO2 dissolves in rainwater, in soils across the planet.
The primary weathering product is carbonate alkalinity, namely bicarbonate (HCO3-) and carbonate (CO3), which is a stable dissolved form of carbon.
Step 3
Carbonate alkalinity is stored in groundwaters and the ocean
Rainwater transports the dissolved carbonate alkalinity away from the field, ultimately ending up in the groundwater and the ocean for long-term storage.
Measuring increased carbonate alkalinity export in the field thereby provides a direct measure of the amount of atmospheric carbon removed.
Enhanced Rock Weathering
Tiny Rocks, Huge Impact
Durable Carbon Removal
Regenerative Agriculture
Highly Scalable
Fostering Climate-Resilience
About Everest
Unified Behind Our Gigaton-Mission
Born from our own frustration with the lack of tools available as former ERW project developers, Everest is commercializing its patent-pending alkalinity sensor to help ERW reach a climate-relevant scale.
Backed by
Small Alkalinity Sensor
Vast Climate Impact
We are on a mission to enable the removal of billions of tons of CO2 from our atmosphere to maintain the habitability of our planet. Join us in building a company that will write climate history!