. . . . . . . . . . "9226353"^^ . . . . "Glikson (krater)"@pl . . . . "-23.98333358764648"^^ . . "Glikson crater is an impact structure (or astrobleme), the eroded remnant of a former impact crater, situated in the Little Sandy Desert of central Western Australia. A possible impact structure was first reported in 1997, and named after Australian geologist A. Y. Glikson, attention to the site being drawn by the presence of a prominent 14 km diameter ring-shaped aeromagnetic anomaly. The area within the ring contains sparse outcrop of uplifted and deformed Neoproterozoic sandstone, but is largely covered by sand dunes. The recent discovery of shatter cones and microscopic shock effects is reliable evidence for an impact origin. Deformation of the sandstone consistent with an impact origin extends out to a diameter of 19 km, which is the best estimate for the original diameter of the original crater. The ring-shaped aeromagnetic anomaly was probably caused by disruption of a horizontal layer of magnetic igneous rock, known as a sill, by the impact event. Nearby outcrops of dolerite have been dated at 508 \u00B1 5 Ma (MiddleCambrian), and if this is the same rock causing the aeromagnetic anomaly, then the impact must be younger, probably of Paleozoic age."@en . . . . . "Confirmed"@en . "Glikson crater"@en . "Glikson Western Australia.jpg"@en . . . . . . . "Landsat image of the area around Glikson crater, the eroded relics of the crater are not clearly visible; screen capture from the NASA World Wind program"@en . "3616"^^ . . . "Yes"@en . "Glikson crater is an impact structure (or astrobleme), the eroded remnant of a former impact crater, situated in the Little Sandy Desert of central Western Australia. A possible impact structure was first reported in 1997, and named after Australian geologist A. Y. Glikson, attention to the site being drawn by the presence of a prominent 14 km diameter ring-shaped aeromagnetic anomaly. The area within the ring contains sparse outcrop of uplifted and deformed Neoproterozoic sandstone, but is largely covered by sand dunes. The recent discovery of shatter cones and microscopic shock effects is reliable evidence for an impact origin. Deformation of the sandstone consistent with an impact origin extends out to a diameter of 19 km, which is the best estimate for the original diameter of the orig"@en . . . . . . . . . . . . . . "994921803"^^ . . . . . . . "Location of the crater in Western Australia"@en . "121.5666656494141"^^ . "Glikson crater"@en . . "POINT(121.56666564941 -23.983333587646)"^^ . . . . . . "No"@en . "Glikson \u2013 krater uderzeniowy na Ma\u0142ej Pustyni Piaszczystej, w stanie Australia Zachodnia. Wiek tego krateru nie jest dobrze znany, powsta\u0142 on w ci\u0105gu ostatnich 508 milion\u00F3w lat (w fanerozoiku). Utworzy\u0142 si\u0119 on w ska\u0142ach krystalicznych pokrytych warstw\u0105 ska\u0142 osadowych. Ska\u0142y przeobra\u017Cone na skutek impaktu ods\u0142aniaj\u0105 si\u0119 na powierzchni ziemi."@pl . . "Glikson \u2013 krater uderzeniowy na Ma\u0142ej Pustyni Piaszczystej, w stanie Australia Zachodnia. Wiek tego krateru nie jest dobrze znany, powsta\u0142 on w ci\u0105gu ostatnich 508 milion\u00F3w lat (w fanerozoiku). Utworzy\u0142 si\u0119 on w ska\u0142ach krystalicznych pokrytych warstw\u0105 ska\u0142 osadowych. Ska\u0142y przeobra\u017Cone na skutek impaktu ods\u0142aniaj\u0105 si\u0119 na powierzchni ziemi."@pl . "-23.983333333333334 121.56666666666666" . . .