Four Craters Lava Field
http://dbpedia.org/resource/Four_Craters_Lava_Field an entity of type: Thing
Four Craters Lava Field is a basaltic volcanic field located south east of Newberry Caldera in the U.S. state of Oregon. The volcanic field covers about 30 square kilometers. Four Pleistocene cinder cones are the source of the flows in the field and are aligned along a fissure trending N 30° W. The cones rise 75 to 120 meters above the flows and the distance between the northernmost and southernmost cones is about 3.5 kilometers.
rdf:langString
rdf:langString
Four Craters Lava Field
rdf:langString
Four Craters Lava Field
rdf:langString
Four Craters Lava Field
xsd:float
43.36000823974609
xsd:float
-120.6626663208008
xsd:integer
17382041
xsd:integer
981219125
rdf:langString
Deschutes & Ochoco National Forests - Crooked River National Grassland
xsd:integer
4924
rdf:langString
FourCraters LeeSiebert 088048.jpg
rdf:langString
Craters of the aptly named Four Craters Lava Field are seen here from the NW on Green Mountain.
xsd:string
43.360009 -120.66267
rdf:langString
Four Craters Lava Field is a basaltic volcanic field located south east of Newberry Caldera in the U.S. state of Oregon. The volcanic field covers about 30 square kilometers. Four Pleistocene cinder cones are the source of the flows in the field and are aligned along a fissure trending N 30° W. The cones rise 75 to 120 meters above the flows and the distance between the northernmost and southernmost cones is about 3.5 kilometers. Closely related to the Four Craters lava field is Crack-in-the-Ground located at the southwest corner of the field. The eruptions from the field were accompanied by a slight sinking of the older rock surface. This shallow, graben-like sink is about 3 kilometers wide and extends to the south into an old lake basin. Crack-in-the-Ground marks the western edge of this small, volcano-tectonic depression and is nearly 9 meters deep and over a meter wide. The crack is the result of a tension fracture along a hingeline produced by the draping of Green Mountain lava flows over the edge of upthrown side of the concealed fault zone.
<second>
1.57788E12
xsd:gYear
0050
xsd:nonNegativeInteger
4044
xsd:double
1500.8352
<Geometry>
POINT(-120.6626663208 43.360008239746)