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Physiographic Map of Lava Butte ^ Jefferson Primary Route the Surface of the Earth and the Vegetation and Structures on It

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Physiographic Map of Lava Butte ^ Jefferson Primary Route the Surface of the Earth and the Vegetation and Structures on It NE Revere Ave 850000 1080000 1090000 1100000 1110000 ¤£20 850000 Central Oregon Pilot Butte Community Elevation: 4,139 ft. College ¤£20 NW Wall St NE Greenwood Ave NW Newport Ave NE Franklin Ave Chamber of Commerce ^_ 840000 Pilot Butte, named in 1851, is a cinder cone butte that rises nearlyBear Creek 500 Rd feet above the NW Galveston Ave Des Chutes Museum ^_ surrounding plains. It makes Bend one of three cities in the continental U.S. to have an extinct volcano within its city limits. Old Bend 1110000 SW Century Dr Century SW SE 15th St SW Simpson Ave Old Mill District The Old Mill District is a vibrant area of shopping, dining, and entertainment located in the heart of the city. It was originally a massive Brooks-Scanlon sawmill complex that began lumber production in 1916. The mill was open and active until 1994. er iv s R Reed Market Rd ute Desch Broken Top Club 840000 ¤£97 830000 Bend Parkway 1070000 Tetherow Golf Club Bend Golf & Country Club SW Century Dr 830000 China Hat Rd Knott Rd 820000 r e v i R s e t u h c s e D Widgi Golf Club Lost Track Golf Club Baker Lake Seventh Mountain Resort Assuming a paved road 24 feet wide and 6 inches thick, there is enough rock in the 820000 flow to pave 160,000 miles of road. This is equivalent to a paved road circling the world six and a half times. BURLINGTON NORTHERN ¤£97 Lava Island Falls ^_ 810000 Dillon Falls ^_ High Desert The volume of rock in the Lava Butte Lava Flow Museum is 380,000,000 cubic yards. The flow spilled into ^_ the Deschutes River forming lava dams in some places and shoving the river westward out of its channel in others. 810000 NEWBERRY NATIONAL Benham Falls ^_ VOLCANIC MONUMENT The long straight cliffs that run diagonally across the 800000 map are fault scarps. Fault scarps form when a fault moves during a strong earthquake, and one side rises a few feet above the other. These scarps are the result of dozens of earthquakes that have occurred over the last 100,000 years or more. One fault runs directly beneath Lava Butte and probably served as a path for the rising magma that fed the Lava Butte eruption. 800000 790000 Lava Butte Deschutes River Elevation: 5,970 ft. N¸ Two miles of railroad grade across the Lava Butte lava flow were constructed in late 1931 during a two month period. The first train used the new section of railroad on April 7, 1932. Burlington Northern continues to use this railroad today. The Lava Butte cinder cone erupted 7,000 years ago and covered over nine square miles with lava. The butte offers a panoramic view of central Oregon, including a spectacular view of the Cascade Range and the northwest flank of Newberry. Lava Lands ^_ Visitor Center ¤£97 790000 1070000 1080000 1090000 1100000 STATE OF OREGON Explanation: The lidar data used to create this map were collected from a light Legend DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES aircraft carrying a highly accurate laser scanner. The scanner makes over 100,000 Railroad OREGON VICKI S. McCONNELL, STATE GEOLOGIST Point of Interest measurements each second to build up a three-dimensional “point cloud” model of Physiographic Map of Lava Butte ^_ Jefferson Primary Route the surface of the earth and the vegetation and structures on it. A computer sorts Bend Urban Growth Boundary E O L O G G Y A Secondary Route ¤£20 97 F ¤£ N O D the points, separating those that measure the ground from those that measure T N M Newberry National Volcanic Monument I E N Linn 126 M E ¤£ T R R A trees and buildings. Images derived from these sets of points are then merged with Deschutes County, Oregon A L P Water I E N D D other forms of digital data to create this map. The inset maps of Lava Butte show U N S O T G R E I R E a 3D perspective with derivative lidar products and orthophotos. 2011 S O Bend Cartography: Rachel Lyles, Oregon Department of Geology and Mineral Industries Lane Crook 1937 2 0 0 7 The Oregon Department of Geology and Mineral Industries (DOGAMI) has been collecting lidar data in Oregon since 2006. The goal is to cover the entire state as OPEN-FILE REPORT O-11-04 Map projection: Oregon Lambert, HARN NAD83 Datum, International Feet funding for the data collection becomes available. You can learn more about lidar Disclaimer: This map is not intended to provide authoritative locations for any of ¤£97 and view lidar images of other parts of Oregon at: www.OregonGeology.org the features depicted. Although it is derived from highly accurate lidar imagery, Deschutes ¤£20 it should not be used for engineering or survey purposes. Data sources: Lidar from DOGAMI and the Oregon Lidar Consortium (2010). National Agriculture Klamath For copies of this publication contact: Imagery Program (NAIP) orthophotos from the U.S. Department of Agriculture (2009). Street and railroad 0 0.5 1 Lake Nature of the Northwest Information Center data from Esri (2008). Bend urban growth boundary from the Department of Land Conservation and Kilometer 800 NE Oregon Street #28, Suite 965 ® Development (2009). Waterbodies from the Pacific Northwest Hydrography Framework partnership (2005). Portland, Oregon 97232 telephone (971) 673-2331 Newberry National Volcanic Monument boundary from the U.S. Forest Service. All water, street, and rail 0 0.5 1 http://www.NatureNW.org data were spatially corrected by DOGAMI using the lidar data. Mile.
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