Mineralica 2026-1

The Great Andean Bird and the Stones: Agates from San Rafael, Argentina

Cite

Cite this article

Short link

mineralica.com/a/5s0r2r

Print

Johann Zenz (2026): The Great Andean Bird and the Stones: Agates from San Rafael, Argentina. Mineralica 2026-1, pp. 6–20.

Online

Johann Zenz (2026): The Great Andean Bird and the Stones: Agates from San Rafael, Argentina. Mineralica online, February 2026. https://mineralica.com/a/5s0r2r (accessed October 13, 2026)

Agates from San Rafael in Argentina's Mendoza province are among the most colorful in the world. Johann Zenz presents their localities and special features and tells the controversial story of their discovery.

Agate with a so-called turtle back structure from San Rafael. 9.8 cm. Pat McMahan collection and photo.

Agates from the province of Mendoza in central western Argentina have been available on the market in large quantities since the mid-1990s and remain among the most sought-after agates worldwide. This article aims to provide a closer look at these colorful cryptocrystalline quartz varieties, including their interesting discovery history and the current collecting situation.

Location, climate, and economy

The province of Mendoza, known throughout Europe and the USA primarily for its excellent wines, is located in central Argentina and borders Chile to the west. Much of the landscape consists of typical dry steppe, occasionally interspersed with small sandy deserts. In the western part, the rugged mountain landscape of the Andes is impressive, with the most famous and highest peak in America, the 6,961 m high Aconcagua (a former volcano), towering majestically near the border with Chile.

The province of Mendoza, divided into 18 departments, has a dry, continental climate with large differences between day and night, fairly warm summer months, cold winter months, and rather low rainfall.

The most important cities were mostly built around the former oases near Mendoza City, Guaymallén, Las Heras, and Godoy Cruz. The small town of Malargüe, also known among collectors for its sedimentary agate deposits (“Puma agates”), is located in the sparsely populated south of the province.

Agate from the San Rafael area with an unusual color combination and a pronounced flow channel in the lower right area. 10 cm. Hannes Holzmann collection, Albert Russ photo.
Intense chromatography phenomenon (color zone changes independent of the band systems). 6.3 cm. Pat McMahan collection and photo.

As already mentioned, wine, with Malbec as its most important variety, is Mendoza's most significant export. In addition, agriculture is practiced and some oil is produced. The province is particularly important from a transport perspective as the “gateway to Chile.”

The city of San Rafael is located in the central south of the province at the foot of the Andes and near the Rio Atuel, which is impressive for its emerald green waters. In the wider vicinity of San Rafael, there are numerous agate deposits that still provide excellent agates in relatively large quantities.

Geological situation

The province of Mendoza can be divided into three major geological zones: the Precordillera-Cordillera Frontal, the Cordillera Principal, and the Coastal Cordillera. The Precordillera-Cordillera Frontal zone (also known as the San Rafael Block) is particularly important for the agate deposits around San Rafael. It is mainly composed of early to late Paleozoic sediments, some of which were brought back to the surface during subduction and uplift processes in the late Miocene and Pliocene. The western part of these sediments was severely deformed in the Devonian period. In addition, there are Precambrian to early Paleozoic metamorphic rocks. These ancient rocks are overlaid by andesitic-rhyolitic volcanic layers of the Choiyoi/Cochicó Group, which are mainly exposed in the San Rafael Block. Carboniferous and Triassic granites occur in between in all locations. The San Rafael block is known for particularly violent and prolonged tectonic and volcanic activity (Mogessie et al., 1999). Andesitic lava, rhyolitic tuffs and ignimbrites, as well as trachytes and keratophyric lavas, are particularly prevalent, lying on top of older layers from the Carboniferous and Early Permian periods. These are themselves partially overlaid by sediments from the Middle and Late Permian periods. South of the Rio Atuel, a series of different sedimentary and volcanic rocks from the Tertiary and Quaternary periods can be observed (Cingolani & Ramos, 2017).

The exciting history of the discovery

No other agate deposit in the world has caused such intense discussion and conflict among collectors as that of San Rafael. The reason for this is incorrect information about the location of the deposit, which unfortunately can still be found in some relevant publications today.

The well-known gemstone company Ruppenthal in Idar-Oberstein has been offering rough agates from Argentina, clearly originating from the San Rafael region, for sale in large quantities since the late 1970s. The German-Argentine mineral dealer Diego Weber first brought agates from San Rafael to the Munich Mineral Show as merchandise in the early 1980s – with the correct location information. An accurate account of the chronology of the interesting discovery history of the San Rafael agates can be found in Mayer (2015).

In 1993, agates from San Rafael were offered for sale in the USA for the first time by Luis de los Santos, a former Argentine actor who now lives in the USA. He gave these agates the trade name “Condor agates” (after the mighty ruler of the skies in the Andes region, the South American condor), which is still popular …

In Mineralica 2026-1

This article runs on pages 6–20. The first 2 pages are free to browse.

View all

Mineralica 2026-1

Tourmalines of the Island of Elba

Elba is the type locality of elbaite and was the world's most famous tourmaline locality in the 19th century. Antonio Miglioli describes the geology, historic localities, colors and characteristic terminations of Elba tourmalines.

By Antonio Miglioli

Mineralica 2026-1

The Kaiserbründl Locality on the Gratlspitze, Tyrol

Ore was already mined at the Kaiserbründl on the Gratlspitze in Tyrol in the Bronze Age. Thomas Wimmer came for the colorful lapidary material and found a wealth of colorful micro-minerals on the dumps.

By Thomas Wimmer

Mineralica 2026-3

Diamond: The Making and Unmaking of the “King of Gems”

Growth, dissolution and erosion leave traces on diamond crystals that a good loupe already reveals. Erwin Geiss explains what these surfaces tell us about the journey up from deep inside the Earth.

By Erwin Geiss