. . . . . . . . . . . "Lassen and Shasta counties, California, U.S."@en . . . . . . . "Le Cinder Cone est un volcan de type c\u00F4ne volcanique situ\u00E9 au nord de la Californie dans le parc national volcanique de Lassen sur le territoire des comt\u00E9s de Lassen et Shasta."@fr . . . . "2101.9008"^^ . . "Trail hike"@en . . . . . . . . . . . . . . . . . . . . . . . . . "1114084703"^^ . "Cinder Cone"@en . . . . . . . "Prospect Peak"@en . . . . . "-121.3199996948242"^^ . . . . . . "Cinder Cone"@en . . . . . . . "Cinder Cone"@fr . . . . "Le Cinder Cone est un volcan de type c\u00F4ne volcanique situ\u00E9 au nord de la Californie dans le parc national volcanique de Lassen sur le territoire des comt\u00E9s de Lassen et Shasta."@fr . . . . "345258"^^ . . . . "Cinder Cone and the Fantastic Lava Beds"@en . . . . . "Cinder Cone is a cinder cone volcano in Lassen Volcanic National Park within the United States. It is located about 10 mi (16 km) northeast of Lassen Peak and provides an excellent view of Brokeoff Mountain, Lassen Peak, and Chaos Crags."@en . . . "POINT(-121.31999969482 40.547500610352)"^^ . . . . . . "Cinder Cone is a cinder cone volcano in Lassen Volcanic National Park within the United States. It is located about 10 mi (16 km) northeast of Lassen Peak and provides an excellent view of Brokeoff Mountain, Lassen Peak, and Chaos Crags. The cone was built to a height of 750 ft (230 m) above the surrounding area and spread ash over 30 sq mi (78 km2). Then, like many cinder cones, it was snuffed out when several basalt lava flows erupted from its base. These flows, called the Fantastic Lava Beds, spread northeast and southwest, and dammed creeks, first creating Snag Lake on the south and then Butte Lake to the north. Butte Lake is fed by water from Snag Lake seeping through the lava beds. Nobles Emigrant Trail goes around Snag Lake and follows the edge of the lava beds. Its age has been controversial since the 1870s, when many people thought it was only a few decades old. Later, the cone and associated lava flows were thought to have formed about 1700 or during a 300-year- long series of eruptions ending in 1851. Recent studies by U.S. Geological Survey (USGS) scientists, working in cooperation with the National Park Service to better understand volcanic hazards in the Lassen area, have firmly established that Cinder Cone was formed during two eruptions that occurred in the 1650s."@en . . . . . . . . . . . . . . . . "40.54750061035156"^^ . . "Cinder Cone at Lassen Volcanic National Park.jpg"@en . . . "256"^^ . . "Cinder Cone is a 748-foot high cone of loose scoria"@en . . . . . "Cinder Cone is een sintelkegelvulkaan in Lassen Volcanic National Park in het noorden van de Amerikaanse staat Californi\u00EB. De vulkaan ligt zo'n 16 km ten noordoosten van Lassen Peak. Zoals het geval is bij veel andere sintelkegelvulkanen, doofde Cinder Cone uit toen er basaltlava uit de basis van de vulkaan stroomde. Die stromen zijn de en bevinden zich rond Cinder Cone in het noordoosten en zuidwesten. De kegel zelf rijst zo'n 230 meter boven het omliggende landschap uit en biedt een panorama van Lassen, Mount Tehama en Chaos Crags."@nl . . . . . "Cinder Cone"@nl . "1666"^^ . . . . . . . . . . . . . "6896"^^ . . . . . . . . . . "Cinder Cone is een sintelkegelvulkaan in Lassen Volcanic National Park in het noorden van de Amerikaanse staat Californi\u00EB. De vulkaan ligt zo'n 16 km ten noordoosten van Lassen Peak. Zoals het geval is bij veel andere sintelkegelvulkanen, doofde Cinder Cone uit toen er basaltlava uit de basis van de vulkaan stroomde. Die stromen zijn de en bevinden zich rond Cinder Cone in het noordoosten en zuidwesten. De kegel zelf rijst zo'n 230 meter boven het omliggende landschap uit en biedt een panorama van Lassen, Mount Tehama en Chaos Crags."@nl . "40.5475 -121.32" . . "1666"^^ . . . "Extinct Cinder cone"@en . . . . . . . . . . . . "21335"^^ . .