Merume River | |
---|---|
Location | |
Country | Guyana |
Physical characteristics | |
Mouth | Kamarang River |
The Merume River is a river of Guyana, a tributary of the Kamarang River.
Merume is also the name of a nearby mountain, [1] which is 30 miles east of Mount Roraima. [2] Director Creek is a tributary of Merume River. First Falls is a feature of the river which also limits travel by boat. [3]
Merumite was discovered in 1937 appearing as black grains among diamonds and gold in the river gravel. [3] In 1958, merumite was determined to be a complex aggregate of eskolaite and chromium, X-ray diffraction data showed it contained eskolaite, guyanaite, bracewellite, grimaldiite, and mcconnellite. [4]
Kamakusa was a settlement along the river, and formerly a government center. [3]
The Geography of Guyana comprises the physical characteristics of the country in Northern South America and part of Caribbean South America, bordering the North Atlantic Ocean, between Suriname and Venezuela, with a land area of approximately 214,969 square km. The country is situated between 1 and 9 north latitude and between 56 and 62 west longitude. With a 459 km (285 mi)-long Atlantic coastline on the northeast, Guyana is bounded by Venezuela on the west, Brazil on the west and south, and Suriname on the east.
The Guiana Shield is one of the three cratons of the South American Plate. It is a 1.7 billion-year-old Precambrian geological formation in northeast South America that forms a portion of the northern coast. The higher elevations on the shield are called the Guiana Highlands, which is where the table-like mountains called tepuis are found. The Guiana Highlands are also the source of some of the world's most well-known waterfalls such as Angel Falls, Kaieteur Falls and Cuquenan Falls.
Roraima is one of the 26 states of Brazil. Located in the country's North Region, it is the northernmost and most geographically and logistically isolated state in Brazil. It is bordered by the state of Pará to the southeast, Amazonas to the south and west, Venezuela to the north and northwest, and Guyana to the east.
Mount Roraima is the highest of the Pacaraima chain of tepuis or plateaux in South America. It is located at the junction of Brazil, Guyana and Venezuela. A characteristic large flat-topped mountain surrounded by cliffs 400–1,000 m (1,300–3,300 ft) high. The highest point of Mount Roraima is located on the southern edge of the cliff at an altitude of 2,810 m (9,220 ft) in Venezuela, and another protrusion at an altitude of 2,772 m (9,094 ft) at the junction of the three countries in the north of the plateau is the highest point in Guyana. The name Mount Roraima came from the native Pemon people. Roroi in the Pemon language means "blue-green", and ma means "great".
The Reedy Glacier is a major glacier in Antarctica, over 100 nautical miles long and 6 to 12 nautical miles wide, descending from the polar plateau to the Ross Ice Shelf between the Michigan Plateau and Wisconsin Range in the Transantarctic Mountains. It marks the limits of the Queen Maud Mountains on the west and the Horlick Mountains on the east.
The Mazaruni River is a tributary of the Essequibo River in northern Guyana. Its source is in the remote western forests of the Pakaraima Mountains and its confluence with the Cuyuni River is near Bartica. As it descends from the Guiana Highlands the river runs south-east, past Issano, then northward to Bartica. The river is a source of alluvial gold.
The Pacaraima or Pakaraima Mountains are a mountain range primarily in southwestern Guyana, and into northern Brazil and eastern Venezuela.
The Pomeroon River is located in Guyana, South America, situated between the Orinoco and the Essequibo rivers. The area has long been inhabited by Lokono people. The Pomeroon River is also one of the deepest rivers in Guyana.
The Wai-wai are a Carib-speaking Indigenous people of Guyana and northern Brazil. Their society consists of different lowland forest peoples who have maintained much of their cultural identity with the exception of Christianity which was introduced to them in the late 1950s.
The Ireng River forms part of Guyana's western border with Brazil. It flows through the valleys of the Pakaraima Mountains for most of its length. It is the only major river in Guyana which flows from North to South, up to its confluence into the Takutu River. It is one of the northernmost tributaries of the Amazon river system.
Amaila Falls is located on the Kuribrong River, a tributary of the Potaro River in west central Guyana.
The Ventuari River is the largest tributary of the Orinoco in southern Venezuela. The Ventuari flows from south-central Venezuela in the Guiana Highlands southwest into the Orinoco River. It is 520 km (320 mi) long and its major tributary is the Manapiare River.
The peacock coquette is a species of hummingbird in the "coquettes", tribe Lesbiini of subfamily Lesbiinae. It is found in Brazil, Guyana, and Venezuela.
The Caroaebe River is a river of Roraima state in northern Brazil, near the equator.
The Kaituma River is a river of Guyana in the Barima-Waini region. The mouth is at the upper Barima River, and the area is made up of mostly mangrove swamps.
The Kassikaityu River is a tributary of the Essequibo River of Guyana.
The Rewa River is a river of Guyana. It is a tributary of the Rupununi River.
The Eping River is a tributary of the Kamarang River in Region 8 of Guyana.
The natural range of the carnivorous plant genus Heliamphora is restricted to the southern Venezuelan states of Amazonas and Bolívar, and to adjacent portions of northern Brazil and western Guyana, an area corresponding to the western part of the Guayana Shield. These plants are largely confined to the summits and foothills of the sandstone table-top mountains of the region, known as tepuis.
Guyanaite (CrOOH) is a chromium oxide mineral that forms as an intergrowth with other chromium oxide minerals known as bracewellite (CrOOH) and grimaldiite (CrOOH) as well as eskolaite (Cr2O3) which in early findings were nearly indistinguishable from one another. These oxides formed so closely as intergrowths with one another that they were initially, and erroneously, identified as a single definite mineral previously known as merumite. Because of its complex history and the previously undiscovered nature of these chromium oxide polymorphs, the relevance of any information found in many early experiments involving the mineral formerly known as merumite in regard to guyanaite is unknown and it is implied that in any further reference of merumite it will have been composed of a mineral assemblage including guyanaite. The rare occurrence and complexity from intergrowth of naturally occurring guyanaite hinders experimental work, leading to laboratory synthesized samples which help to better experiment with the minerals.
5°53′N59°53′W / 5.883°N 59.883°W