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  2. Hell's Half Acre Lava Field - Wikipedia

    en.wikipedia.org/wiki/Hell's_Half_Acre_Lava_Field

    The Hell's Half Acre lava plain is located in Bingham and Bonneville counties in the state of Idaho. The site is about 150 square miles (390 km 2) in size. [1] The area where a former lava lake existed is marked by a 875-yard (800 m) long by 328-yard (300 m) wide depression near the summit of the lava field. [7]

  3. Fossickers Way - Wikipedia

    en.wikipedia.org/wiki/Fossickers_Way

    The scenic route draws its name of Fossickers Way due to the many deposits of gold and the variety of gemstones that have been found in the area (mostly by Europeans) since the early 1850s. Prior to this time, local Aboriginal tribes such as the Werawai people of Nundle and its surrounds were known to use local minerals and stones for the ...

  4. Schonchin Butte - Wikipedia

    en.wikipedia.org/wiki/Schonchin_Butte

    The Schonchin Butte Fire Lookout is a fire lookout tower on Schonchin Butte, a cinder cone in Lava Beds National Monument.. The Civilian Conservation Corps built a fire lookout at Schonchin Butte during the summers of 1939 and 1940, as part of federal infrastructure development under the President Franklin D. Roosevelt administration during the Great Depression.

  5. Lava field - Wikipedia

    en.wikipedia.org/wiki/Lava_field

    The two main types of lava field structures are defined as sheet flow lava and pillow lava. Sheet flow lava appears like a wrinkled or folded sheet, while pillow lava is bulbous, and often looks like a pile of pillows atop one another. [2] An important aspect of lava flow morphology is a phenomenon known as lava flow inflation.

  6. Large igneous province - Wikipedia

    en.wikipedia.org/wiki/Large_igneous_province

    In 1992, Coffin and Eldholm initially defined the term "large igneous province" as representing a variety of mafic igneous provinces with areal extent greater than 100,000 km 2 that represented "massive crustal emplacements of predominantly mafic (magnesium- and iron-rich) extrusive and intrusive rock, and originated via processes other than 'normal' seafloor spreading."

  7. Hawaii Route 137 - Wikipedia

    en.wikipedia.org/wiki/Hawaii_Route_137

    The 1990 lava flow that destroyed Kalapana moved along Highway 137. [6] During the 2018 lower Puna eruption of KÄ«lauea's East rift zone, a lava flow from Fissure 20 buried a section of Route 137 between Kamaili Road and Pohoiki Road [ 2 ] and flows from Fissure 8 flowed east across and along Hawaii Route 132 , cutting more of Route 137 in the ...

  8. Google Maps - Wikipedia

    en.wikipedia.org/wiki/Google_Maps

    Google Maps' location tracking is regarded by some as a threat to users' privacy, with Dylan Tweney of VentureBeat writing in August 2014 that "Google is probably logging your location, step by step, via Google Maps", and linked users to Google's location history map, which "lets you see the path you've traced for any given day that your ...

  9. East Lava Field - Wikipedia

    en.wikipedia.org/wiki/East_Lava_Field

    The Squaw Ridge Lava field, also known as the East Lava Field, is a young basaltic field located in the U.S. state of Oregon southeast of Newberry Volcano. [1] The flow erupted from the Lava Mountain shield and is likely related to the Four Craters Lava Field , both of which were created after Mount Mazama erupted.