Two sides to the Kinneret Lake / שתי גדות לכנרת - המשותף והשונה במסלע ובמבנה

Two sides to the Kinneret Lake / שתי גדות לכנרת - המשותף והשונה במסלע ובמבנה

The Sea of Galilee (Kinneret Lake) divides two Neogene basins which are characterized by largely continental clastic sequences and basalt flows. Stratigraphic differences between the two basins are discerned. A comparison of the stratigraphy of both sides of the Sea of Galilee does not support the p...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:אופקים בגיאוגרפיה 1988-01 (25/26), p.7-22
Hauptverfasser: מיכלסון, חיים, פלכסר, עקיבא, ארז, צבי, Michelson, H., Flexer, A., Erez, Z.
Format: Artikel
Sprache:heb
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 22
container_issue 25/26
container_start_page 7
container_title אופקים בגיאוגרפיה
container_volume
creator מיכלסון, חיים
פלכסר, עקיבא
ארז, צבי
Michelson, H.
Flexer, A.
Erez, Z.
description The Sea of Galilee (Kinneret Lake) divides two Neogene basins which are characterized by largely continental clastic sequences and basalt flows. Stratigraphic differences between the two basins are discerned. A comparison of the stratigraphy of both sides of the Sea of Galilee does not support the postulated 107 km left-lateral movement. Although some small strike-slip faults might exist, most faults are of a gravity dip-slip type. A postulated ridge trending NNE, buried under the Sea of Galilee, might have had a stratigraphic influence on sediment distribution between the eastern and western sides. The raw materials, as well as the ores, thermal water and the ground-water of the southern Golan Heights is briefly reviewed too.
format Article
fullrecord <record><control><sourceid>jstor</sourceid><recordid>TN_cdi_jstor_primary_23698535</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><jstor_id>23698535</jstor_id><sourcerecordid>23698535</sourcerecordid><originalsourceid>FETCH-jstor_primary_236985353</originalsourceid><addsrcrecordid>eNqFisEOwUAYhPdAosEjSP4XaDTdreUsRMKx96aJFS1a2d1EPEapgxApLvSF_texFXdzmZlvpkYsh1JmU85Zg7SVih0j5riccYuk_i4FFc2FAp2CXgqYRkkipNAwC1cCuoBvLPEMeMAjnrAEvOIFC3yZaAPmeDMHw_EJxvJvKTAHzMxyN-dHxauSVbxF6otwrUT7503SGY_84cSOlU5lsJXRJpT7wKW9Qd-jHv23fwAHeFwi</addsrcrecordid><sourcetype>Publisher</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Two sides to the Kinneret Lake / שתי גדות לכנרת - המשותף והשונה במסלע ובמבנה</title><source>JSTOR</source><creator>מיכלסון, חיים ; פלכסר, עקיבא ; ארז, צבי ; Michelson, H. ; Flexer, A. ; Erez, Z.</creator><creatorcontrib>מיכלסון, חיים ; פלכסר, עקיבא ; ארז, צבי ; Michelson, H. ; Flexer, A. ; Erez, Z.</creatorcontrib><description>The Sea of Galilee (Kinneret Lake) divides two Neogene basins which are characterized by largely continental clastic sequences and basalt flows. Stratigraphic differences between the two basins are discerned. A comparison of the stratigraphy of both sides of the Sea of Galilee does not support the postulated 107 km left-lateral movement. Although some small strike-slip faults might exist, most faults are of a gravity dip-slip type. A postulated ridge trending NNE, buried under the Sea of Galilee, might have had a stratigraphic influence on sediment distribution between the eastern and western sides. The raw materials, as well as the ores, thermal water and the ground-water of the southern Golan Heights is briefly reviewed too.</description><identifier>ISSN: 0334-3774</identifier><language>heb</language><publisher>חוג לגיאוגרפיה, אוניברסיטת חיפה</publisher><ispartof>אופקים בגיאוגרפיה, 1988-01 (25/26), p.7-22</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/23698535$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/23698535$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,58017,58250</link.rule.ids></links><search><creatorcontrib>מיכלסון, חיים</creatorcontrib><creatorcontrib>פלכסר, עקיבא</creatorcontrib><creatorcontrib>ארז, צבי</creatorcontrib><creatorcontrib>Michelson, H.</creatorcontrib><creatorcontrib>Flexer, A.</creatorcontrib><creatorcontrib>Erez, Z.</creatorcontrib><title>Two sides to the Kinneret Lake / שתי גדות לכנרת - המשותף והשונה במסלע ובמבנה</title><title>אופקים בגיאוגרפיה</title><description>The Sea of Galilee (Kinneret Lake) divides two Neogene basins which are characterized by largely continental clastic sequences and basalt flows. Stratigraphic differences between the two basins are discerned. A comparison of the stratigraphy of both sides of the Sea of Galilee does not support the postulated 107 km left-lateral movement. Although some small strike-slip faults might exist, most faults are of a gravity dip-slip type. A postulated ridge trending NNE, buried under the Sea of Galilee, might have had a stratigraphic influence on sediment distribution between the eastern and western sides. The raw materials, as well as the ores, thermal water and the ground-water of the southern Golan Heights is briefly reviewed too.</description><issn>0334-3774</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1988</creationdate><recordtype>article</recordtype><recordid>eNqFisEOwUAYhPdAosEjSP4XaDTdreUsRMKx96aJFS1a2d1EPEapgxApLvSF_texFXdzmZlvpkYsh1JmU85Zg7SVih0j5riccYuk_i4FFc2FAp2CXgqYRkkipNAwC1cCuoBvLPEMeMAjnrAEvOIFC3yZaAPmeDMHw_EJxvJvKTAHzMxyN-dHxauSVbxF6otwrUT7503SGY_84cSOlU5lsJXRJpT7wKW9Qd-jHv23fwAHeFwi</recordid><startdate>19880101</startdate><enddate>19880101</enddate><creator>מיכלסון, חיים</creator><creator>פלכסר, עקיבא</creator><creator>ארז, צבי</creator><creator>Michelson, H.</creator><creator>Flexer, A.</creator><creator>Erez, Z.</creator><general>חוג לגיאוגרפיה, אוניברסיטת חיפה</general><scope>P.Q</scope></search><sort><creationdate>19880101</creationdate><title>Two sides to the Kinneret Lake / שתי גדות לכנרת - המשותף והשונה במסלע ובמבנה</title><author>מיכלסון, חיים ; פלכסר, עקיבא ; ארז, צבי ; Michelson, H. ; Flexer, A. ; Erez, Z.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-jstor_primary_236985353</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>heb</language><creationdate>1988</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>מיכלסון, חיים</creatorcontrib><creatorcontrib>פלכסר, עקיבא</creatorcontrib><creatorcontrib>ארז, צבי</creatorcontrib><creatorcontrib>Michelson, H.</creatorcontrib><creatorcontrib>Flexer, A.</creatorcontrib><creatorcontrib>Erez, Z.</creatorcontrib><collection>JSTOR Hebrew Journals</collection><jtitle>אופקים בגיאוגרפיה</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>מיכלסון, חיים</au><au>פלכסר, עקיבא</au><au>ארז, צבי</au><au>Michelson, H.</au><au>Flexer, A.</au><au>Erez, Z.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Two sides to the Kinneret Lake / שתי גדות לכנרת - המשותף והשונה במסלע ובמבנה</atitle><jtitle>אופקים בגיאוגרפיה</jtitle><date>1988-01-01</date><risdate>1988</risdate><issue>25/26</issue><spage>7</spage><epage>22</epage><pages>7-22</pages><issn>0334-3774</issn><abstract>The Sea of Galilee (Kinneret Lake) divides two Neogene basins which are characterized by largely continental clastic sequences and basalt flows. Stratigraphic differences between the two basins are discerned. A comparison of the stratigraphy of both sides of the Sea of Galilee does not support the postulated 107 km left-lateral movement. Although some small strike-slip faults might exist, most faults are of a gravity dip-slip type. A postulated ridge trending NNE, buried under the Sea of Galilee, might have had a stratigraphic influence on sediment distribution between the eastern and western sides. The raw materials, as well as the ores, thermal water and the ground-water of the southern Golan Heights is briefly reviewed too.</abstract><pub>חוג לגיאוגרפיה, אוניברסיטת חיפה</pub></addata></record>
fulltext fulltext
identifier ISSN: 0334-3774
ispartof אופקים בגיאוגרפיה, 1988-01 (25/26), p.7-22
issn 0334-3774
language heb
recordid cdi_jstor_primary_23698535
source JSTOR
title Two sides to the Kinneret Lake / שתי גדות לכנרת - המשותף והשונה במסלע ובמבנה
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-20T16%3A51%3A15IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstor&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Two%20sides%20to%20the%20Kinneret%20Lake%20/%20%D7%A9%D7%AA%D7%99%20%D7%92%D7%93%D7%95%D7%AA%20%D7%9C%D7%9B%D7%A0%D7%A8%D7%AA%20-%20%D7%94%D7%9E%D7%A9%D7%95%D7%AA%D7%A3%20%D7%95%D7%94%D7%A9%D7%95%D7%A0%D7%94%20%D7%91%D7%9E%D7%A1%D7%9C%D7%A2%20%D7%95%D7%91%D7%9E%D7%91%D7%A0%D7%94&rft.jtitle=%D7%90%D7%95%D7%A4%D7%A7%D7%99%D7%9D%20%D7%91%D7%92%D7%99%D7%90%D7%95%D7%92%D7%A8%D7%A4%D7%99%D7%94&rft.au=%D7%9E%D7%99%D7%9B%D7%9C%D7%A1%D7%95%D7%9F,%20%D7%97%D7%99%D7%99%D7%9D&rft.date=1988-01-01&rft.issue=25/26&rft.spage=7&rft.epage=22&rft.pages=7-22&rft.issn=0334-3774&rft_id=info:doi/&rft_dat=%3Cjstor%3E23698535%3C/jstor%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rft_jstor_id=23698535&rfr_iscdi=true