Royal Society Volcano
Encyclopedia
The Royal Society Volcano is a large number of basalt
ic cinder cone
s and lava flows are located in the Royal Society Range
of southern Victoria Land
. Most vents are of Quaternary
age. More than 50 basaltic vents, ranging from tiny scoria
mounds to cinder cones up to 300-m high, occupy the foothills of the Royal Society Range. Tephra layers in the ice of Kempe Glacier
, Potassium-Argon
ages as young as 0.08 million years old, and well-preserved geomorphic forms all argued for young, possibly even Holocene
ages.
Basalt
Basalt is a common extrusive volcanic rock. It is usually grey to black and fine-grained due to rapid cooling of lava at the surface of a planet. It may be porphyritic containing larger crystals in a fine matrix, or vesicular, or frothy scoria. Unweathered basalt is black or grey...
ic cinder cone
Cinder cone
According to the , Cinder Cone is the proper name of 1 cinder cone in Canada and 7 cinder cones in the United States:In Canada: Cinder Cone In the United States:...
s and lava flows are located in the Royal Society Range
Royal Society Range
The Royal Society Range is a majestic mountain range in Victoria Land, Antarctica. With its summit at , the massive Mount Lister forms the highest point in this range. Mount Lister is located along the western shore of McMurdo Sound between the Koettlitz, Skelton and Ferrar glaciers...
of southern Victoria Land
Victoria Land
Victoria Land is a region of Antarctica bounded on the east by the Ross Ice Shelf and the Ross Sea and on the west by Oates Land and Wilkes Land. It was discovered by Captain James Clark Ross in January 1841 and named after the UK's Queen Victoria...
. Most vents are of Quaternary
Quaternary
The Quaternary Period is the most recent of the three periods of the Cenozoic Era in the geologic time scale of the ICS. It follows the Neogene Period, spanning 2.588 ± 0.005 million years ago to the present...
age. More than 50 basaltic vents, ranging from tiny scoria
Scoria
Scoria is a volcanic rock containing many holes or vesicles. It is most generally dark in color , and basaltic or andesitic in composition. Scoria is relatively low in mass as a result of its numerous macroscopic ellipsoidal vesicles, but in contrast to pumice, all scoria has a specific gravity...
mounds to cinder cones up to 300-m high, occupy the foothills of the Royal Society Range. Tephra layers in the ice of Kempe Glacier
Kempe Glacier
Kempe Glacier is a short alpine glacier, bounded on the north by Dismal Ridge and on the south by the Mount Kempe-Mount Dromedary ridge, whose chief nourishment is neve fields on the north slopes of Mount Kempe. The glacier drains northeast toward Roaring Valley...
, Potassium-Argon
Potassium-argon dating
Potassium–argon dating or K–Ar dating is a radiometric dating method used in geochronology and archeology. It is based on measurement of the product of the radioactive decay of an isotope of potassium into argon . Potassium is a common element found in many materials, such as micas, clay minerals,...
ages as young as 0.08 million years old, and well-preserved geomorphic forms all argued for young, possibly even Holocene
Holocene
The Holocene is a geological epoch which began at the end of the Pleistocene and continues to the present. The Holocene is part of the Quaternary period. Its name comes from the Greek words and , meaning "entirely recent"...
ages.