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barely scratched the surface"

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Wadi Halfa landscape
Est. 2016 — Khartoum, Sudan

Strategic
Mineral
Exploration.

Partnering with the Republic of Sudan to transform natural resources into mutual prosperity. We find, develop, and own the best assets to deliver sustainable returns.

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"Smashing expectations. Using smart science and creativity to develop one of the world's most profitable gold mines. Opal Mining is on its way to becoming Sudan's next multi-generational, iconic gold producer."

5+

Years
Experience

8

Current
Investments

6

Specialist
Management

4

Experienced
Partners
Minerals in Sudan

Minerals
Potentiality

Sudan is among the largest countries in Africa and characterized with diversified geological units and structure that host great and variable numbers of minerals wealth.

Gold Sample 1
Gold Sample 2

Gold

The area between the Nile and the Red sea, South Kordofan, and South Darfur.

Silver

Red Sea Hills.

Iron & Chromite

Iron at Red Sea Hills. Chromite at Ingessana, Nuba Mountains, Red Sea Hill, and Qala En Nahal.

Manganese & Copper

Red Sea Hills, Bayuda Desert, Ariab Region, and Hofrat En Nahas.

Zinc & Lead

Abu Samar area, Tagoteb, Um Takatik at NE-Nuba Mountains. Lead at Kutum, North Darfur.

Limestone & Marbles

Bayuda, Red Sea Hills, coastal plane, and North Port Sudan (Gypsum).

Black Sands

Red Sea Coastal (contains magnetite, ilmenite, rutile, and zircon).

Additional

Agricultural (Phosphate), Kaoline, Talc, Magnesite, Feldspars, Fluorspar, Barite, White Gold.

Value Proposition

Why Opal
Mining?

Why Opal Mining

We Invest Early

Fearless & Educated

30+ Years Experience

Leaders in Startup Inv.

4+ Countries Active

Focus on Yield

Concession Coordinates

Block NS-R2
Northern State (Wadi Halfa)

Opal Mining Co. Ltd signed concession agreement for the exploration, development and exploitation of gold and association metals.

Concession location preview
Surveyed Area

Sahara Desert

~300 sq. km

Coordinates Bounded

Lat 21°20'25" – 21°12'37"
Lon 31°42'0.00" – 31°30'0.00"

Logistical Access

Khartoum to Abu Hamad (470km) via National Hwy.
Abu Hamad to Wadi Halfa (Station 6) (165km) via Railway.
Station 6 to Concession (55km) via Unpaved Road (4x4).
Total Distance: ~690km.

Physiography & Climate

The concession area domain is situated in the western margin of the Nubian Desert, whereby more than 50% of the surface area is covered by sand dunes. The thickness of the sandy sheets varies from place to place, but in most localities reaches a few meters above the surrounding. Most of the ridges and basement inselbergs are scattered in this area. Low-lying basement outcrops are exposed as peneplains. The topography of the south of the Block is covered by low-lying Nubian Sandstones.

The concession is part of the Sahara Desert and thus the prevailing climate is dry with less than 50mm per year rainfall in the period from July to September. The winter season is from November to February in which the daily temperature may drop to 15°C. Otherwise, the climate is very dry and hot, the daily mean temperature ranges from 35°C to 42°C.

Tectonic Setting & Geology

The Precambrian geology in NE Africa comprises two distinct crustal domains; The Nile Craton and the Arabian-Nubian Shield (Stern, 1994; Kröner, et al. 1987a; Vail, 1983; 1988; Rocci, 1965).

Geology of Wadi Halfa-Bayuda-Gabgaba area

The area covered by Bayuda Desert is relatively well studied compared to other areas in northern Sudan (Vail, 1971; Barth and Meinhold, 1979; Dawoud, 1980; Ries, et al, 1985). Wadi Halfa and Bayuda Terrains (Schandelmeier, et al, 1994) represent the reworked eastern foreland of the Nile Craton, while Gabgaba Terrain (Abdelrahman, 1993) represented the westernmost part of the Arabian-Nubian Shield (ANS). Wadi Halfa area poorly understood due to the limited studies conducted in the area (Stern, et al, 1994; Griffiths, et al, 1987).

According to previous studies in north and northeast Sudan, the litho-stratigraphic units of the Wadi Halfa-Bayuda-Gabgaba area are (Denkler, et al, 1994; Abdelrahman, 1993; Vail, 1988; Barth and Meinhold, 1979):

  • 01 Phanerozoic sediments (youngest)
  • 02 Magmatic rocks
  • 03 Molasse – type sediments
  • 04 Volcano-sedimentary sequences
  • 05 Ophiolitic mélange rocks
  • 06 Low-grade metasediments
  • 07 High-grade supra-crustal metasediments
  • 08 High-grade gneisses (oldest)
Concession Map
Fig 1. Location Block
Geological Map
Fig 2. Geological Data
Milestone Event

Concession
Agreement

Ministry of Minerals, Khartoum.
Official signing ceremony securing exploration rights.

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Team at mining place
Our Growth Engine

"We believe that we've only
barely scratched the surface"

Executive Board

Our Leadership

Ahmad Chakik

Ahmad Chakik

Chairman & Founder

Over 3 decades experience in Investment, Mining and Financial Management across Africa and the UAE. Extensive strategic links to China, the Middle East, and Asia forming the foundation of Opal Mining.

Dr. Mohamed Kharrubi

Dr. Mohamed Kharrubi

Director

Executive with extensive experience across the UN, USA, Malaysia, Libya, UAE, and South Africa. Expertise in corporate strategy across diverse international disciplines and cultures.

Yoro Mohamed Diallo

Yoro M. Diallo

Financial Manager

Prominent banker and strategist to African governments and multi-billion dollar corporations. Managed >US$600 million of donor flows at Citibank across multiple African nations.

Aygun Aliyeva

Aygun Aliyeva

Legal Dept. Manager

Legal expert holding direct memberships in international bar associations spanning the EU and Asia. Founding partner of deep cross-continental legal consortiums.

Esam Ibrahim

Esam Ibrahim

IT & Cloud Specialist

20+ years driving global IT operations. Technical architect specializing in secure remote infrastructure, ensuring robust and compliant data networks for continuous corporate operations.

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Direct Communication

Connect
With Us

Headquarters

Al Sayid Ali Al Merghani Street
Khartoum North (Bahri), Sudan.

General Inquiries

chakik@consultant.com

Mobile

00249991959595

WhatsApp

00905449601119