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Aton Resources
Aton Resources Inc. (TSX.V: AAN) is a Canadian listed exploration company principally focused on advancing the Rodruin and Hamama mineral exploration projects in the Eastern Desert of Egypt (located within the Arabian-Nubian Shield). It has offices in Vancouver, Canada, and Cairo, Egypt. Tonno Vahk took over as interim president and chief executive officer in October 2021. It is listed on the TSX Venture Exchange under the ticker TSXV:AAN. Operations The company holds mineral concessions at Abu Marawat. The Abu Marawat Concession was previously controlled by Centamin and was subsequently awarded to Alexander Nubia as part of the international bid round. The concessions are located in close proximity to excellent infrastructure (near to railway, seaport, high tension electricity grid and the major cities of Qena and Safaga). Within the Abu Marawat Concession are several different deposits representing different geological environments: # Abu Marawat: a mesothermal gold-copper vei ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Desert
The Eastern Desert (Archaically known as Arabia or the Arabian Desert) is the part of the Sahara desert that is located east of the Nile river. It spans of North-Eastern Africa and is bordered by the Nile river to the west and the Red Sea and Gulf of Suez to the east. It extends through Egypt, Eritrea, Sudan and Ethiopia. The Eastern Desert is also known as the Red Sea Hills. The Desert consists of a mountain range which runs parallel to the coast, wide sedimentary plateaus extending from either side of the mountains and the Red Sea coast. The rainfall, climate, vegetation and animal life sustained in the desert varies between these different regions.The Desert has been a mining site for building materials, and precious and semi-precious metals throughout history. It has historically contained many trade routes leading to and from the Red Sea, including the Suez Canal. Geography Historical formation Between 100 and 35 million years ago the area that is now the Eastern D ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arabian-Nubian Shield
The Arabian-Nubian Shield (ANS) is an exposure of Precambrian crystalline rocks on the flanks of the Red Sea. The crystalline rocks are mostly Neoproterozoic in age. Geographically - and from north to south - the ANS includes parts of Israel, Jordan, Egypt, Saudi Arabia, Sudan, Eritrea, Ethiopia, Yemen, and Somalia. The ANS in the north is exposed as part of the Sahara Desert and Arabian Desert, and in the south in the Ethiopian Highlands, Asir province of Arabia and Yemen Highlands. The ANS was the site of some of man's earliest geologic efforts, principally by the ancient Egyptians to extract gold from the rocks of Egypt and NE Sudan. This was the most easily worked of all metals and does not tarnish. All of the gold deposits in Egypt and northern Sudan were found and exploited by Egyptians. The earliest preserved geologic map was made in 1150 BCE to show the location of gold deposits in Eastern Egypt; it is known as the Turin papyrus. New gold discoveries have been ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Centamin
Centamin plc (, ) is a gold mining company focused on the Arabian-Nubian Shield. It has offices in London, UK; Mount Pleasant, Western Australia; and Alexandria, Egypt. Its registered office is in Jersey. It is listed on the London Stock Exchange and the Toronto Stock Exchange and is a constituent of the FTSE 250 Index. History Centamin was first listed on the Australian Stock Exchange in 1970.Centamin Egypt – 12 million ounces of gold and rising Proactive Investors, 29 August 2008 In 1999 it acquired Pharaoh Gold Mines, a company that had been exploring for gold in since 1995, and became "Centamin Egypt". [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Qena
Qena ( ar, قنا ' , locally: ; cop, ⲕⲱⲛⲏ ''Konē'') is a city in Upper Egypt, and the capital of the Qena Governorate. Situated on the east bank of the Nile, it was known in antiquity as Kaine (Greek Καινή, meaning "new (city)"; Latinized transliteration: Caene) and Maximianopolis. Gauthier identifies Qena with ancient Shabt. Overview This provincial capital is located about 95 km from El Balyana and 63 km north of Luxor. It is most famous for its proximity to the ruins of Dendara. It owes its modern prosperity to the opening of the Wadi Qena towards the Red Sea, which is a major traffic route between Upper Egypt and the Red Sea. Tourists traveling between Luxor and the Red Sea will assuredly pass through this city since there is only one good road connection. Qena is noted for its pottery. Qena is also known for its beautiful huge mountains and green nature. Qena also has one of the highest concentration of Coptic Christians in Egypt (approximately 35% of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Safaga
Port Safaga, also known as Safaga ( ar, سفاجا ', ), is a town in Egypt, on the coast of the Red Sea, located south of Hurghada. This small port is also a tourist area that consists of several bungalows and rest houses, including the Safaga Hotel, with a capacity of 48 rooms (126 beds). Having numerous phosphate mines, it is regarded as the phosphates export center. A paved road of connects Safaga to Qena of Upper Egypt. History The town was founded between 282 BC and 268 BC, by Satyrus ( grc, Σάτυρος). It was called Philotera ( grc, Φιλωτέρα) in honor of the deceased sister of the Pharaoh Ptolemy II Philadelphus. Stephanus of Byzantium write that it was also called Philoterida ( grc, Φιλωτερίδα). Safaga City is considered one of the most important therapeutic tourist centres, as special medical researches have proved the potential of attracting international tourism to Safaga. Safaga was a merchant port for many years. The town has a small to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesothermal
In climatology, the term mesothermal is used to refer to certain forms of climate found typically in the Earth's temperate zones. It has a moderate span of temperature, with winters not cold enough to sustain snow cover. Summers are warm within oceanic climate regimes, and hot within continental or subtropical climate regimes. Origin of term The term is derived from two Greek words meaning "having a moderate amount of heat." This can be misinterpreted, however, since the term is actually intended to describe only the temperature conditions that prevail during the winter months, rather than those for the year as a whole. Definition Under the original Köppen climate classification, all places with an average temperature in their coldest month that is colder than 18°C, but warmer than −3°C, are said to have a mesothermal climate. The isotherm of -3°C for the coldest monthly mean temperature, was observed to be the line where the climate was likely cold enough to support a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanogenic Massive Sulfide Ore Deposit
Volcanogenic massive sulfide ore deposits, also known as VMS ore deposits, are a type of metal sulfide ore deposit, mainly copper-zinc which are associated with and created by volcanic-associated hydrothermal events in submarine environments. These deposits are also sometimes called volcanic-hosted massive sulfide (VHMS) deposits. The density generally is 4500 kg/m3. They are predominantly stratiform accumulations of sulfide minerals that precipitate from hydrothermal fluids on or below the seafloor in a wide range of ancient and modern geological settings. In modern oceans they are synonymous with sulfurous plumes called black smokers. They occur within environments dominated by volcanic or volcanic derived (e.g., volcano-sedimentary) rocks, and the deposits are coeval and coincident with the formation of said volcanic rocks. As a class, they represent a significant source of the world's copper, zinc, lead, gold and silver ores, with cobalt, tin, barium, sulfur, selenium, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Porphyry Copper Deposit
Porphyry copper deposits are copper ore bodies that are formed from hydrothermal fluids that originate from a voluminous magma chamber several kilometers below the deposit itself. Predating or associated with those fluids are vertical dikes of porphyritic intrusive rocks from which this deposit type derives its name. In later stages, circulating meteoric fluids may interact with the magmatic fluids. Successive envelopes of hydrothermal alteration typically enclose a core of disseminated ore minerals in often stockwork-forming hairline fractures and veins. Because of their large volume, porphyry orebodies can be economic from copper concentrations as low as 0.15% copper and can have economic amounts of by-products such as molybdenum, silver, and gold. In some mines, those metals are the main product. The first mining of low-grade copper porphyry deposits from large open pits coincided roughly with the introduction of steam shovels, the construction of railroads, and a surge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
