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  2. Kimberlite - Wikipedia

    en.wikipedia.org/wiki/Kimberlite

    False-color scanning electron microscope image of kimberlite from South Africa. Olivine crystals (green) are in a fine-grained matrix made up of clay minerals and carbonates (presented in blue, purple and buff colors). Kimberlite is an igneous rock and a rare variant of peridotite. It is most commonly known to be the main host matrix for diamonds.

  3. Lake Henshaw - Wikipedia

    en.wikipedia.org/wiki/Lake_Henshaw

    Lake Henshaw is a reservoir in San Diego County, California, at the southeast base of Palomar Mountain, approximately 70 miles (110 km) northeast of San Diego and 100 miles (160 km) southeast of Los Angeles.

  4. Northern Alberta kimberlite province - Wikipedia

    en.wikipedia.org/wiki/Northern_Alberta...

    The NAKP kimberlite fields are located about 350 km (220 mi) to 450 km (280 mi) north to northwest of Edmonton in an area bounded by 55° and 57°N latitude and 115° and 118°W longitude. The area lies within the Canadian boreal forest and is sparsely settled.

  5. Geography of California - Wikipedia

    en.wikipedia.org/wiki/Geography_of_California

    Map of California topography and geomorphic provinces California's major mountain ranges. California is a U.S. state on the western coast of North America.Covering an area of 163,696 sq mi (423,970 km 2), California is among the most geographically diverse states.

  6. Lake Ellen Kimberlite - Wikipedia

    en.wikipedia.org/wiki/Lake_Ellen_Kimberlite

    The Lake Ellen Kimberlite is a poorly exposed volcanic breccia located about 10 miles (16 km) northeast of Crystal Falls in the Upper Peninsula of Michigan. The first publication in 1981 [ 1 ] describing the feature led to speculation that this or similar kimberlites in the area might have been the source of the diamonds discovered a century ...

  7. Buffalo Head Hills kimberlite field - Wikipedia

    en.wikipedia.org/wiki/Buffalo_Head_Hills...

    Deep beneath the BHH kimberlite field lies a 2.0 to 2.4 billion year old Precambrian craton called the Buffalo Head terrane, which has no exposure at surface.The Precambrian craton is overlain by about 1,600 m (5,200 ft) of Paleozoic and Mesozoic sedimentary rocks, which are covered by as much as 200 m (660 ft) of unconsolidated glacial and post-glacial sediments of Quaternary age.

  8. Attawapiskat kimberlite field - Wikipedia

    en.wikipedia.org/wiki/Attawapiskat_kimberlite_field

    The Attawapiskat kimberlite field is a field of kimberlite pipes located astride the Attawapiskat River in the Hudson Bay Lowlands, in Northern Ontario, Canada.It is thought to have formed about 180 million years ago in the Jurassic period when the North American Plate moved westward over a centre of upwelling magma called the New England hotspot, also referred to as the Great Meteor hotspot.

  9. Cuyama Valley - Wikipedia

    en.wikipedia.org/wiki/Cuyama_Valley

    Cuyama seen from the east, on SR-166. The valley encompasses an area of approximately 300 square miles (780 km 2).It is bounded on all sides by mountains: the Sierra Madre Mountains along the south and west, La Panza Range on the north, and Caliente Range along the northeast − all of the California Coast Ranges System; and the San Emigdio Mountains on the east − of the Transverse Ranges ...