Gratomic Inc.
GRAT
Rank in Stocks
#35012
Gratomic Inc. operates as a junior mineral exploration company primarily... Gratomic Inc. operates as a junior mineral exploration company primarily engaged in acquiring and developing mineral assets. While its core exploration activities are concentrated in Canada and Namibia, the company also holds properties in Brazil. Its exploration efforts target a diverse range of commodities, including base metals, rare metals, industrial minerals, and precious metals. A significant asset is its wholly-owned Aukam graphite project in southern Namibia's Karas Region (Bethanie district), encompassing approximately 137,473 hectares. Additionally, Gratomic possesses full ownership of the Buckingham graphite property in Quebec, Canada, which consists of eight claim blocks spanning roughly 480 hectares. The company's portfolio further includes the 100%-owned Capim Grosso Property in Capim Grosso, Brazil, covering an area of 426.03 hectares. Originally established in 2007, the company operated under the name CKR Carbon Corporation before rebranding to Gratomic Inc. in December 2017. Its corporate headquarters are situated in Toronto, Canada.
Share Price
$0.02186342
Last synced: 2025-06-03
Market Cap
$4.38M
Change (1 day)
-0.04%
Change (1 year)
35.36%
Country
CA
Trade Gratomic Inc. (GRAT)
Category
Basic Materials
Stock split history for Gratomic Inc. (GRAT)
Gratomic Inc. stock (symbol: GRAT) underwent a total of 0 stock splits.
The most recent stock split occurred on Oct 19, 2026.
One GRAT share bought prior to Oct 19, 2026 would equal to 0 GRAT shares today.
The most recent stock split occurred on Oct 19, 2026.
One GRAT share bought prior to Oct 19, 2026 would equal to 0 GRAT shares today.
Stock split list
| Year | Split | Multiple | Cumulative Multiple |
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| Not enough data for the provided dates. | |||
Stock splits for similar companies or competitors
| Company | Number of stock splits | Cumulative Multiple | Country |
|---|---|---|---|
| 4 | x2 |
AU
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| 0 | - |
MX
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| 3 | x3 |
SA
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| 0 | - |
BR
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| 0 | - |
CN
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