{"id":214,"date":"2015-07-22T18:16:05","date_gmt":"2015-07-22T17:16:05","guid":{"rendered":"http:\/\/marine.geophysicsgpr.com\/?page_id=214"},"modified":"2017-03-10T19:51:54","modified_gmt":"2017-03-10T18:51:54","slug":"bottom-sub-bottom-mapping","status":"publish","type":"page","link":"https:\/\/marine.geophysicsgpr.com\/en\/marine-geophysics-applications\/environmental\/bottom-sub-bottom-mapping","title":{"rendered":"Bottom &amp; Sub-bottom Mapping"},"content":{"rendered":"<div id=\"pl-214\"  class=\"panel-layout\" ><div id=\"pg-214-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-214-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-214-0-0-0\" 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-214-0-0-0\" ><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 <span style=\"color: #317671\"><a href=\"mailto:info@geophysicsgpr.com\">Marine Survey Team<\/a><\/span>.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-214-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-214-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-214-1-0-0\" class=\"so-panel widget widget_sow-image panel-first-child panel-last-child\" data-index=\"1\" ><div class=\"panel-widget-style panel-widget-style-for-214-1-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-214\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_applications_bottom-mapping_inset.jpg\" width=\"225\" height=\"305\" srcset=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_applications_bottom-mapping_inset.jpg 225w, https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_applications_bottom-mapping_inset-221x300.jpg 221w\" sizes=\"auto, (max-width: 225px) 100vw, 225px\" title=\"Marine_applications_bottom mapping_inset\" alt=\"Sub-bottom Mapping\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><div id=\"pgc-214-1-1\"  class=\"panel-grid-cell\" ><div id=\"panel-214-1-1-0\" class=\"so-panel widget widget_sow-image panel-first-child panel-last-child\" data-index=\"2\" ><div class=\"panel-widget-style panel-widget-style-for-214-1-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-214\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_Applications_Bottom-mapping.jpg\" width=\"640\" height=\"402\" srcset=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_Applications_Bottom-mapping.jpg 640w, https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_Applications_Bottom-mapping-300x188.jpg 300w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" title=\"Marine_Applications_Bottom mapping\" alt=\"Sub-bottom Mapping\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\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\/environmental\/bottom-sub-bottom-mapping\" class=\"more-link\" title=\"Read Bottom &amp; Sub-bottom Mapping\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":78,"parent":170,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-214","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/214","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=214"}],"version-history":[{"count":20,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/214\/revisions"}],"predecessor-version":[{"id":1597,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/214\/revisions\/1597"}],"up":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/170"}],"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=214"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}