Pyramid Formation | |
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Stratigraphic range: | |
![]() The Pyramid consists of Pyramid Formation trachyte | |
Type | Geological formation [1] |
Unit of | Mount Edziza volcanic complex [2] |
Underlies | Ice Peak Formation, Edziza Formation [1] |
Overlies | Nido Formation [1] |
Lithology | |
Primary | Trachyte, comendite, pantellerite [1] |
Other | Basalt [1] |
Location | |
Coordinates | 57°30′N130°36′W / 57.5°N 130.6°W [2] |
Region | British Columbia [1] |
Country | Canada [1] |
Type section | |
Named for | The Pyramid [1] |
Named by | Souther et al. [3] |
Year defined | 1984 [3] |
![]() Cross section showing the maximum extent of the Pyramid Formation at the end of Pyramid time |
The Pyramid Formation is a stratigraphic unit of Pleistocene age in northwestern British Columbia, Canada.
The Pyramid Formation takes its name from The Pyramid, a prominent pyramid-shaped lava dome on the northeastern flank of Mount Edziza. [1] [4]
Two subunits comprise the Pyramid Formation. The lower unit is a basal pyroclastic member up to 3 m (9.8 ft) thick. It contains trachytic pumice, sodic pyroxene and alkali feldspar; the latter two are present in the form of lithic clasts and crystals. This unit is rusty brown in colour and was deposited by a pyroclastic surge. The upper unit consists of a basalt member up to 65 m (213 ft) thick. It includes 6 to 10 individual basalt flows that reach thicknesses of 3–20 m (9.8–65.6 ft). They appear to have been deposited almost immediately after the pyroclastic surge was erupted. [1] Several silicic lava domes and minor lava flows of the Pyramid Formation postdate the basalt member. Among the silicic domes are Sphinx Dome, Pharaoh Dome and The Pyramid. [5]
The Pyramid Formation has a volume of 11.4 km3 (2.7 cu mi), making it the eighth most voluminous geological formation of the Mount Edziza volcanic complex after the Little Iskut Formation. [1] [2] It overlies the Nido Formation and underlies the Ice Peak and Edziza formations, all of which have formed in the last 8 million years. K–Ar dating of the Pyramid Formation has yielded ages of 1.2 ± 0.4 million years and 1.20 ± 0.03 million years for comenditic glass and 0.94 ± 0.12 million years and 0.94 ± 0.05 million years for trachyte. [1]