Chile

LLAMARA Project

The Llamara Project is the first Chilean multi-element deposit composed of magnesium and lithium clays, plus potassium salts, strontium and other minerals destined mainly for the electromobility market and the production of photocatalytic green hydrogen.

The Project is located in the westernmost part of the lithium triangle, between the regions of Antofagasta and Tarapacá, at an average height of 850 meters above sea level and in the area with the highest solar radiation on the planet.





With over 50,000 Hectares, legaly manifested, with a complete NI43-101 Geological Study and drillings executed.

The Llamara Salt Flat is located 25 km west of the highway and 30 km from the Loa River, in the city of Iquique.

The project consists of 10 properties registered in the Pozo Almonte mining conservatory.

ENVIRONMENTAL Crisis

"We need to change the way we do and see the world. As a project we are committed to climate change and life, and we want this new way of doing things to change the course of our land for the benefit of future generations."

Carlos Araya

Llamara Group SpA

SUSTAINABLE Development

The Llamara project is a Technological revolution that seeks to generate a change of mentality in the industry, taking mining to a higher level of environmental awareness and social responsibility

Carlos Araya

Llamara Group SpA

New ENGINEERING

We will reduce by 95% the carbon footprint of the first two links of the production chain of electromobility, such as mining extraction and chemical processing.

Carlos Araya

Llamara Group SpA



Isabella GOLD

The prospect is made up of five exploitation concessions, covering a total area of ​​1,056 hectares.

• Isabella Prospect, located in the Alto del Buitre sector, Hualañé and Licantén communes, Curicó Province, Maule Region, Chile.

• The work carried out by the undersigned on the prospectus includes the review of the existing literature, chemical analysis certificates, mining property records, verification of mineralized structures in the field and geochemical sampling of mineralized sectors to verify the existence of reported grades.

• From a geological point of view, the prospect can be classified as a deposit composed of veined gold and silver structures, associated with intrusive rocks of Upper Paleozoic age belonging to the Coastal Range, the prospect can be classified as a low-sulfidation Isabella epithermal deposit.

• The Coastal Range is composed of a mixture of intrusives, metasediments and volcanic rocks from the Upper Paleozoic to the Mesozoic, forming a strip of at least 60 km wide and which extends from north to south along the western margin of the Coastal Range. Central Chile.

Isabella Gold

• Geological mapping, rock geochemistry
• Geological reports.
• Magnetic lifting.
• Reconnaissance tunnels and small-scale gold mining.
• Trenches.
• DDH drilling.
• NI 43-101 Report

• These rocks contain a series of quartz veins with significant gold and silver contents. Additionally, it is also possible to locate structurally controlled breccias that contain significant polymetallic gold mineralization and silver.

• Isabella is currently NI 43-101 compliant, the Indicated Resource estimate for this prospect is 259,200 tons grading an average of 5.74 g/t gold, equivalent to 47,383 oz of gold.




ROSALINDA Project

The mine is located in Cajón del Maipo, in the commune of San José de Maipo, 76 km from Santiago and north of the town of San Gabriel. It is part of the old Merceditas mining district, which produced silver in colonial times and later copper. At its peak, Minera Merceditas produced more than 40% of the copper produced in Chile.

The objective of this visit was to recognize the geology of the area, the mineralization and its extension along with the mining development. To date there is no mining activity and most of the works have partial access. The UTM coordinates of the center of the mineralized area are N 6.258.200 – E 389.900 near the Volcán River.

ROSALINDA Project

Mineralization: The mineralization observed in the mining works is sulfide, constituting a mantle contained in a gray tuff; it consists of chalcopyrite, arsenopyrite, danaite and pyrite, extending as fine dissemination and in small clusters. In some areas, magnetite is abundant, as well as specularite.
Along with the mineralization, the rock presents quartz banding and a slight sillification.

Mining Workings: During the visit, 7 mining workings were recognized, some of 60 m, others of 20-25 m, partially accessible. There are others that are covered by alluvial fill.
Even though the area is covered with bushes and shrubs, it is possible to see large clearings, the product of an old mining operation.

Mining Property: The Rosalinda mining property is covered by the exploitation concession called Rosalinda 1/10; It covers an area of ​​96 hectares and belongs to the Melosita Uno Society of San José de Maipo.