scholarly journals Radiocarbon Dates for Lava Flows from Northeast Rift Zone of Mauna Loa Volcano, Hilo 7 1/2’ Quadrangle, Island of Hawaii

Radiocarbon ◽  
1989 ◽  
Vol 31 (2) ◽  
pp. 179-186 ◽  
Author(s):  
J M Buchanan-Banks ◽  
J P Lockwood ◽  
Meyer Rubin

Twenty-eight 14C analyses are reported for carbonized roots and other plant material collected from beneath 15 prehistoric lava flows erupted from the northeast rift zone (NERZ) of Mauna Loa Volcano (ML) utilizing the recovery techniques of Lockwood and Lipman (1980). Most samples were collected from the Hilo 7 1/2’ quadrangle during field work for a geologic map of that quadrangle (Buchanan-Banks, unpub data); a few sample sites are located in adjacent quadrangles: Piihonua to the west and Mountain View to the south. Altitudes are given in English units as well as metric to facilitate locating sites on USGS topographic maps.

Radiocarbon ◽  
1979 ◽  
Vol 21 (2) ◽  
pp. 306-320 ◽  
Author(s):  
M L Kelley ◽  
E C Spiker ◽  
P W Lipman ◽  
J P Lockwood ◽  
R T Holcomb ◽  
...  

Ninety-six new 14C dates are reported for carbonized roots and other plant material coll from beneath prehistoric lava flows and ash deposits from Mauna Loa (ML) and Kilauea volcanoes. Before 1976, only 10 flows from these volcanoes had been dated by radiocarbon methods. Collection of dateable material has been facilitated by an improved understanding of the conditions of charcoal formation and preservation beneath basaltic lavas (Lockwood & Lipman, 1979).


1985 ◽  
Vol 125 ◽  
pp. 64-66
Author(s):  
L.M Larsen ◽  
T Tukiainen

During the 1984 field work in the Motzfeldt Centre of the Igaliko Complex, some of the remnants of the supracrustal rocks of the Eriksfjord Formation were investigated. These occur at several localities bordering the centre, and are also found as inclusions (roof rafts) of variable size within the syenites of the centre. These supracrustal rocks form the easternmost extension ofthe sandstones and lavas ofthe Eriksfjord Formation, the major part of which is found on the Narssaq peninsula to the west. Some of the easterly remnants were described by Emeleus & Harry (1970) who noted the occurrence ofsandstone and volcanic breccia, agglomerate and lava flows and described two small agglomerate-filled volcanic plugs. Our observations extend those of Emeleus & Harry (1970).


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