@BGS.50k.Superficial.deposits OBJECTID;Shape;LEX;LEX_RCS_I;LEX_RCS_D;MAX_TIME_D;MIN_TIME_D;BGSREF;VERSION;RELEASED;NOM_BGS_YR;LEX_RCS;MAX_PERIOD;MIN_PERIOD;TYPE_D;BROAD_D;SETTING_D;LEX_WEB;LEX_D;RCS;RCS_X;RCS_D;RCS_ORIGIN;RANK;BED_EQ_D;MB_EQ_D;FM_EQ_D;SUBGP_EQ_D;GP_EQ_D;SUPGP_EQ_D;MAX_AGE;MAX_EPOCH;MAX_SUBPER;MAX_ERA;MAX_EON;BGSTYPE;SET_PLUS_D;ENVIRONM_D;BGSRED;BGSGREEN;BGSBLUE;MAP_SRC;MAP_WEB;NOM_SCALE;UUID;GUID;USAGE;INFO; 169279;Polygon;RT13;11199999_RT13-XSV;River Terrace Deposits, 13-Sand and gravel;Quaternary Period;Quaternary Period;503;9.25;31-03-2025;1991;RT13-XSV;Quaternary;Quaternary;superficial deposits;sand and gravel;rivers (U);https://webapps.bgs.ac.uk/lexicon/lexicon.cfm?pub=RT13;River Terrace Deposits, 13;XSV;S + V;Sand and gravel;Sedimentary;Litho-morpho-genetic;Not Applicable;Not Applicable;Not Applicable;Not Applicable;Not Applicable;Not Applicable;Not Defined;Not Defined;Not Defined;Cenozoic;Phanerozoic;Superficial;with older river deposits, where the original upper surface is now higher than today's floodplain;These sedimentary deposits are fluvial in origin. They are detrital, ranging from coarse- to fine-grained and form beds and lenses of deposits reflecting the channels, floodplains and levees of a river or estuary (if in a coastal setting).;255;201;148;ew329_Bournemouth;https://webapps.bgs.ac.uk/data/MapsPortal/series.html?series=E50k&collection=PMAP&filter=Bournemouth;50000;bgsn:BGSGeology50_V9_1004081045529372;88a2b28b-9003-462d-bafc-3fd362bc81dc;© UKRI www.bgs.ac.uk/ipr;www.bgs.ac.uk/products/digitalmaps/digmapgb_50.html;