{"id":247,"date":"2015-08-06T15:30:47","date_gmt":"2015-08-06T14:30:47","guid":{"rendered":"http:\/\/marine.geophysicsgpr.com\/?page_id=247"},"modified":"2017-03-10T19:55:10","modified_gmt":"2017-03-10T18:55:10","slug":"bottom-and-sub-bottom-mapping","status":"publish","type":"page","link":"https:\/\/marine.geophysicsgpr.com\/en\/marine-geophysics-applications\/geological-and-geotechnical\/bottom-and-sub-bottom-mapping","title":{"rendered":"Bottom and Sub-bottom Mapping"},"content":{"rendered":"<div id=\"pl-247\"  class=\"panel-layout\" ><div id=\"pg-247-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-247-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-247-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div class=\"texte-home-right article panel-widget-style panel-widget-style-for-247-0-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h4>Bottom and sub-bottom mapping employ numerous marine geophysical techniques.<\/h4>\n<ul>\n<li>Bathymetry and side scan sonar surveys can be used to map\u00a0the bottom of lakes, rivers,\u00a0ponds and seas.<\/li>\n<li class=\"h2resize\">Sub-bottom mapping can identify layers' thicknesses and provide estimates of debris\/sediment accumulation and bedrock depths.<\/li>\n<li class=\"h2resize\">Sediment sampling can be used to produce maps of bottom sediment types;<\/li>\n<li class=\"h2resize\">Underwater imaging can be used to produce maps of bottom vegetation and fish habitats.\u00a0<\/li>\n<\/ul>\n<p>For more information on the techniques applied, following the links below :<\/p>\n<ul>\n<li><a href=\"http:\/\/marine.geophysicsgpr.com\/techniques\/bathymetry\">Bathymetry;<\/a><\/li>\n<li><a href=\"http:\/\/marine.geophysicsgpr.com\/techniques\/side-scan-sonar\">Side scan sonar;<\/a><\/li>\n<li><a href=\"http:\/\/marine.geophysicsgpr.com\/en\/marine-geophysics-techniques\/sediment-water-sampling-and-underwater-imaging\">Sediment Sampling;<\/a><\/li>\n<li><a href=\"http:\/\/marine.geophysicsgpr.com\/techniques\/sub-bottom-profiling\">Sub-bottom profiling.<\/a><\/li>\n<\/ul>\n<p>For more information, please contact our <a class=\"mail-link\" href=\"mailto:info@geophysicsgpr.com\">Marine Survey Team<\/a>.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Bottom and sub-bottom mapping employ numerous marine geophysical techniques.Bathymetry and side scan sonar surveys can be used to map\u00a0the bottom of lakes, rivers,\u00a0ponds and seas.Sub-bottom mapping can identify layers&#8217; thicknesses and provide estimates of debris\/sediment accumulation and bedrock depths.Sediment sampling can be used to produce maps of bottom sediment types;Underwater imaging can be used to&#8230;  <a href=\"https:\/\/marine.geophysicsgpr.com\/en\/marine-geophysics-applications\/geological-and-geotechnical\/bottom-and-sub-bottom-mapping\" class=\"more-link\" title=\"Read Bottom and Sub-bottom Mapping\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":78,"parent":176,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-247","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/247","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/comments?post=247"}],"version-history":[{"count":16,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/247\/revisions"}],"predecessor-version":[{"id":1666,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/247\/revisions\/1666"}],"up":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/176"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/media\/78"}],"wp:attachment":[{"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/media?parent=247"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}