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All of the objects are located in the Monoceros constellation and are located about 720 parsecs or 2,300 light-years from Earth. [2] Due to its relative proximity and large size, it is extremely well-studied. [6] NGC 2264 is sometimes referred to as the Christmas Tree Cluster and the Cone Nebula.
The Cone Nebula is an H II region in the constellation of Monoceros. It was discovered by William Herschel on December 26, 1785, at which time he designated it H V.27. The nebula is located about 830 parsecs or 2,700 light-years from Earth .
A tuff cone, sometimes called an ash cone, is a small monogenetic volcanic cone produced by phreatic (hydrovolcanic) explosions directly associated with magma brought to the surface through a conduit from a deep-seated magma reservoir. They are characterized by high rims that have a maximum relief of 100–800 meters (330–2,620 ft) above the ...
A conical hill (also cone or conical mountain) is a landform with a distinctly conical shape. It is usually isolated or rises above other surrounding foothills, and is often of volcanic origin. Conical hills or mountains occur in different shapes and are not necessarily geometrically-shaped cones; some are more tower-shaped or have an ...
This hemisphere contains approximately 68% of Earth's landmass and is home to about 90% of the global population. [4] It includes North America, Europe, Asia, and most of Africa. Southern Hemisphere: The half that lies south of the Equator. It contains approximately 32% of Earth's landmass and is home to about 10% of the global population.
Tennena Cone, alternatively Icebridge Cone, is a small volcanic cone in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of 2,390 metres (7,840 feet) and lies on the upper western flank of Ice Peak , the prominent south peak of Mount Edziza .
The "cone of death," also known as the "cone of uncertainty," has traditionally focused on coastal areas and the projected path of tropical storms or hurricanes, including timing and wind-related ...
The cone contains a circular, 45-metre-deep (148-foot) summit crater and was the source of an extensive lava flow that travelled down the northern side of the Big Raven Plateau towards Buckley Lake. Eve Cone is surrounded by a number of other volcanic features, including Tsekone Ridge, Pillow Ridge, Sidas Cone and the Triplex Cones.