Diamond-producing countries

Евразия
Индия
С доистори- ческих времен
II век
1829/1930
Китай
до XX века
1958
1968
Россия
XVIII век первая половина
1938
1953
Борнео
Нет данных
VI-VII вв.
Нет данных
Северная Америка
Канада
1920
Нет данных
1991
США
1843
Нет данных
1906
Южная Америка
Бразилия
XVII век
1725
1977
Венесуэлла
1913
1931
Нет данных
Гайана
Нет данных
Нет данных
Нет данных
Фр. Гвиана
Нет данных
Нет данных
Нет данных
Австралия
 
1851
1867
1976
Африка
Ангола
С конца XVI в.
1912
1952
Ботсвана
1955
Нет данных
1967
Габон
1945
1945
Нет данных
Гана
1919
1921
Нет данных
Гвинея
1932
1932
1953
ДР Конго
1903
1913
1946
Зимбабве
1903
1903
1907
Кот д'Ивуар
1919
1946
Отсутствуют
Лесото
1860-е
Нет данных
1955
Либерия
1911
1932
Отсутствуют
Мали
1955
1955
1956
Намибия
1908
1908
Нет данных
Сьерра-Леоне
1930
1932
Нет данных
Танзания
1913
1913
1940
Того
Нет данных
1932
Нет данных
ЦАР
1914
1914
Нет данных
ЮАР
1866
1870
1870
Условные обозначения
Добыча в 2021 году
Открытие первой промышленной алмазоносной россыпи
Первое открытие коренного промышленного источника алмазов
Первая находка алмаза
Цвет алмаза
бесцветные
черные
коричневые
серые
оранжевые
красные
голубые
зеленые
сине-зеленые
шампань
розовые
пурпурно-красные
фиолетово-розовые
желтоватые
различных оттенков (D-Z)

In nature, diamond occurs mainly in the form of separate well-formed crystals of octahedral, rhombododecahedral, cubic shape, less often in the form of crystalline aggregates.
The main indigenous industrial sources of diamonds are kimberlites and lamproites – alkaline-ultrabasic rocks of ancient platforms, forming mainly tube-shaped bodies, dikes and veins, rarely sills, characterized by vertical and subvertical occurrence. The main objects of production are tubes.
The share of gemstones in indigenous diamond deposits varies widely: from 2-5% (Diesel in Zaire and Argyle in Australia) to 70% (Majgawan in India).

Another type of diamond deposits are placers. They make up a fairly small part of the world's stone production (up to 10%). However, the share of jewelry raw materials extracted from them is quite high, which determines their industrial importance.

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