Raw emerald stones from Swat, Pakistan. Photography: Deng Kaiyin; Copyright © Guild Gem Laboratory.
Faceted gemstone of vivid green emerald from Swat, Pakistan. Photography: Deng Kaiyin; Copyright © Guild Gem Laboratory.
Explore the Mining Area History
The Swat Valley in Pakistan is one of the earliest known emerald mining areas to mankind, with a history spanning over a thousand years. In 2000, when French scientists Giuliani et al. were sorting out the ancient French royal jewels, they conducted an oxygen isotope analysis on the emeralds inlaid on a pair of ancient Roman earrings dating back 2,500 years to trace their origin. The research results confirmed that they originated from the Swat Valley in Pakistan (Giuliani, 2000). Considering the prosperity of the Gandhara Kingdom* at that time, it can be inferred that as early as BC, people had already started mining Swat emeralds and spreading them along the Silk Road, much earlier than the discovery and use of Colombian emeralds.
The geographical location of Pakistan. The pictures are sourced from the Internet.
Due to the abandonment of the Silk Road, the emerald mines in Pakistan were gradually forgotten and once disappeared from the scene. It was not until 1958 that local shepherds accidentally discovered this verdant treasure on a hillside and presented it to the then crown prince. Only then did the Swat emerald shine on the world stage again. The four main emerald mining areas in Pakistan are the Swat Valley, Malak and Mohmand, Bajaur, and Khaltaro. Among them, the most important Swat Valley is located on the southern edge of the Hindu Kush Mountains, which is an extension of the Himalayas. Some of the mining sites with the largest production in this mining area are scattered along the northeastern border of Mingora Town. The harsh climate conditions have greatly increased the difficulty of emerald mining. For more than 70 years, the local people have been safeguarding this natural treasure using the most primitive manual mining methods. Since 1960, the Pakistani government has started to control the exploitation of the newly discovered mines in the Himalayas.
The intact crystal shape, rich color and high clarity make this bag of emeralds from Pakistan highly valuable.
Photography: Andrew Lucas; Copyright © Guild Gemology Education.
Since the 1970s, the Swat emerald deposit in Pakistan has gradually become one of the important production areas of high - quality emeralds in the world. The output increased from 5,000 carats in 1978 - 1979 to 40,000 carats in 1987 - 1988, with 40% being high - quality or extremely high - quality emeralds (Kazmi et al., 1989). Among the total 400,000 carats of emeralds produced during 1996 - 1999, 60% - 70% were high - quality emeralds (Khan and Kausar, 2010).
The core area of the Gandhara Kingdom includes the eastern part of present - day Afghanistan and the northwestern part of Pakistan. It is located in the Hindu Kush Mountains, and most of its population lives in the valleys formed by the alluvial of rivers such as the Kabul River, the Swat River, and the Indus River.
Overview of Mine Geology
Regional Geological Map of the Swat Area in Pakistan (Adapted from Kazmi et al., 1984)
The most important Swat mining area in Pakistan. The picture is provided by Mr. Hayat from Pakistan.
Local miners are extracting emeralds in the tunnel. The picture is provided by Mr. Hayat from Pakistan.
Emeralds can be seen on the ground of the mine pit. Their green color forms a sharp contrast with the light gray of the parent rock.
The picture is provided by Mr. Hayat from Pakistan.
Ore containing emeralds. The picture is provided by Mr. Hayat from Pakistan.
Basic Properties
The bright green rough Swat emeralds from Pakistan mostly take the form of hexagonal prisms
and have a relatively high degree of euhedral crystal.
Photography: Deng Kaiyin; Copyright © Guild Gem Laboratory.
Cut - faceted Swat emeralds from Pakistan. Photography: Deng Kaiyin; Copyright © Guild Gem Laboratory.
Mr. Andrew Lucas, hailed as the "Father of Field Gems", commented on Pakistani emeralds as follows: "They have the best color, a scarce output, and the most distinctive feature is that even very small grains have a rich color." The colors of Swat emeralds from Pakistan are mostly green - blue - green, with highly saturated bright green visible. Their main coloring elements are Cr, V, and Fe. Compared with emeralds from other origins, the emeralds in this region have a medium - to - high Fe content, a relatively high Cr content, and a medium V content (the carbonatized and altered ultrabasic parent rock may provide a large amount of Cr elements for the formation of Swat emeralds in Pakistan). Among them, the high Cr content is presumed to be the main reason for the high saturation of the emeralds in this region. When the Fe content is high, it may cause a blue - tint and suppress fluorescence.
Comparison of Cr contents in emeralds from different origins. Swat emeralds from Pakistan have a significantly relatively high Cr content.
In the ultraviolet - visible light absorption spectrum, the selective absorption of light by coloring elements can be seen: The broad absorption band centered at 850nm is caused by Fe2+; the broad absorption bands centered at 430nm and 620nm, as well as the weak absorption peaks at 630nm and 680nm, are related to Cr3+; the weak absorption peak at 378nm is caused by Fe3+. No obvious absorption peak of V is visible.
The emerald - green color makes Swat emeralds from Pakistan fascinating, and their inner world is equally wonderful. Inside, there are commonly sickle - shaped, tadpole - shaped, and rain - filament - shaped two - phase gas - liquid inclusions, as well as solid mineral inclusions such as magnesite, calcite, pyrite, limonite, black spinel, mica, and quartz. In addition, clear hexagonal color bands, tubular inclusions, and dendritic inclusions can also be seen. Similar to the oil - drop effect presented inside Colombian emeralds, this rare optical effect can also be observed in Swat emeralds.
Two - phase inclusion; Field of view: 1.53 mm. Photography: Sun Xueying; Copyright © Guild Gem Laboratory.
Rhombohedral or granular carbonate mineral inclusions; Field of view: 1.51 mm. Photography: Sun Xueying; Copyright © Guild Gem Laboratory.
Tubular inclusions; Field of view: 1.09 mm. Photography: Sun Xueying; Copyright © Guild Gem Laboratory.
Special Variety - Trapiche Emerald
Trapiche emeralds are usually found in Colombia. Recently the authors received six emeralds reportedly from Swat Valley, Pakistan, polished as double-sided wafers, retaining their original hexagonal crystal habit and exhibiting a trapiche-like pattern.
These samples weighed from 0.38 to 0.83 ct, with a refractive index of 1.588–1.599 and a birefringence of 0.009–0.011.
Generally, these trapiche emeralds were composed of four parts from rim to core: a green rim, a light green area, six arms, and a colorless core, as illustrated. The rims had a highly saturated green color, and most were relatively clean except for several fractures and tiny fluid inclusions. The rims ranged from approximately 1 to 2 mm wide. Although the boundary between the green rim and the light area was not very sharp, a hexagonal boundary was visible. Six black arms spread in a hexagonal symmetric pattern, with each arm perpendicular to the hexagonal side. The colorless core usually had a hexagonal shape.
Microscopic observation revealed that every arm contained many minute black platy inclusions. These small particles appeared dark under transmitted light , while they showed bright metallic luster under reflected light. Micro - Raman analyses identified these inclusions as magnetite. Peaks at 662 and 545 cm–1 were consistent with two main peaks of magnetite, according to the RRUFF online database (rruff.info), while peaks at 683 and 400 cm–1 may be assigned to the emerald host.
Chemical analysis by energy - dispersive X - ray fluorescence (EDXRF) on the sample shown in figure 19 revealed an iron content of 20,860 ppm (n = 3) in the light green area and 17,000 ppm (n = 3) in the rim. The difference in iron content may be due to the inclusions, since magnetite (Fe₃O₄) is mainly composed of iron and oxygen.
They range from 0.83 to 0.38 ct from left to right, with a thickness of about 1.51 to 2.08 mm. Photo by Kaiyin Deng.
The trapiche emeralds from Pakistan were mainly composed of four parts: a green rim, a light green area, six arms, and a nearly colorless core as illustrated in figure A. These arms appear dark under transmitted light (B) and show bright metallic luster under reflected light (C); field of view 8.48 mm. Illustration and photos by Yujie Gao.
Raman analysis identified these inclusions as magnetite. Peaks at 662 and 545 cm⁻¹ agree with the two main peaks of magnetite, according to the RRUFF database, while peaks at 683 and 400 cm⁻¹ may be assigned to the emerald host.
Application of Swat Emeralds in the Luxury Goods Market
As one of the five most precious gemstones, emeralds have always been sought - after by royalty in Western society. There are many legendary pieces of jewelry in history, such as the Catherine Crown, Empress Josephine's emerald necklace, the Delhi Durbar necklace and short - necklace, all of which show people's preference for emeralds. The vivid and dark green Swat emeralds usually have a small grain size, and most faceted finished products are less than 1 carat. With the continuous combination of jewelry and watchmaking techniques, inspired by the natural beauty of emeralds, European luxury watch and jewelry companies have purchased a large number of small - sized emeralds from Pakistan and used them in watchmaking. After meticulous carving, they give people a strong visual impact.
Report of Swat Pakistan emeralds - sample
Acknowledgements:
Thanks to Mr. Hayat from Pakistan for providing the mine - area pictures, and thanks to Kaiyin Deng and Yizhi Zhao for taking some of the pictures.
Authors of this article: Xueying Sun, Yujie Gao
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