"Chisel marks" on columnar joint face

The sides of any columns in columnar jointing do not form a single uniform fracture, rather they grow incrementally. Each subhorizontal fracture increment, known as a "chisel mark," has its own fracture surface markings that indicate the direction of growth of that fracture. Most fractures...

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Bibliographic Details
Other Authors: Wojtal, Steven F.
Format: Other/Unknown Material
Language:unknown
Published: Oberlin College Library 1997
Subjects:
Online Access:http://server15963.contentdm.oclc.org/u?/p15963coll1,1697
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spelling ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/1697 2023-05-15T16:47:56+02:00 "Chisel marks" on columnar joint face Wojtal, Steven F. Zone: 28, Easting: 403467, Northing: 7101612 64.02783 -16.9758 Skaftafell National Park Iceland Austurland Quaternary 1997-08 jpeg2000 http://server15963.contentdm.oclc.org/u?/p15963coll1,1697 unknown Oberlin College Library wojtals_pcd_104 http://server15963.contentdm.oclc.org/u?/p15963coll1,1697 For research and educational use only. For all other uses please contact the Oberlin College. Geology Department 35 mm Kodachrome slide. Oberlin College. Geology Department. Geology Structural Joints (Geology) Columnar joints Basalt. 1997 ftohiocolleges 2022-05-18T11:55:36Z The sides of any columns in columnar jointing do not form a single uniform fracture, rather they grow incrementally. Each subhorizontal fracture increment, known as a "chisel mark," has its own fracture surface markings that indicate the direction of growth of that fracture. Most fractures here propagated from left to right across the column face, and most of these fractures initiated along the lower edge of the chisel mark. Other/Unknown Material Iceland Five Colleges of Ohio Digital Collections Austurland ENVELOPE(-15.650,-15.650,64.267,64.267) Skaftafell ENVELOPE(-16.940,-16.940,63.999,63.999)
institution Open Polar
collection Five Colleges of Ohio Digital Collections
op_collection_id ftohiocolleges
language unknown
topic Geology
Structural
Joints (Geology)
Columnar joints
spellingShingle Geology
Structural
Joints (Geology)
Columnar joints
"Chisel marks" on columnar joint face
topic_facet Geology
Structural
Joints (Geology)
Columnar joints
description The sides of any columns in columnar jointing do not form a single uniform fracture, rather they grow incrementally. Each subhorizontal fracture increment, known as a "chisel mark," has its own fracture surface markings that indicate the direction of growth of that fracture. Most fractures here propagated from left to right across the column face, and most of these fractures initiated along the lower edge of the chisel mark.
author2 Wojtal, Steven F.
format Other/Unknown Material
title "Chisel marks" on columnar joint face
title_short "Chisel marks" on columnar joint face
title_full "Chisel marks" on columnar joint face
title_fullStr "Chisel marks" on columnar joint face
title_full_unstemmed "Chisel marks" on columnar joint face
title_sort "chisel marks" on columnar joint face
publisher Oberlin College Library
publishDate 1997
url http://server15963.contentdm.oclc.org/u?/p15963coll1,1697
op_coverage Zone: 28, Easting: 403467, Northing: 7101612
64.02783
-16.9758
Skaftafell National Park
Iceland
Austurland
Quaternary
long_lat ENVELOPE(-15.650,-15.650,64.267,64.267)
ENVELOPE(-16.940,-16.940,63.999,63.999)
geographic Austurland
Skaftafell
geographic_facet Austurland
Skaftafell
genre Iceland
genre_facet Iceland
op_source 35 mm Kodachrome slide. Oberlin College. Geology Department.
op_relation wojtals_pcd_104
http://server15963.contentdm.oclc.org/u?/p15963coll1,1697
op_rights For research and educational use only. For all other uses please contact the Oberlin College. Geology Department
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