The previous page is sending you to https://www.alamy.com/the-geology-of-the-goldfields-of-british-guiana-epidote-granitite-gneiss-x-12tikuru-essequibo-river-fhutu-hy-j-williams-diorite-gneiss-x-30tupeku-mazaruni-river-ihulu-li-j-williams-the-fetrografhy-of-the-fundamental-gneissose-complex-35-on-the-amucura-lliver-wanaparn-ou-the-barima-river-arimu-creekin-the-cuyuni-river-parawakas-rapids-on-the-mazaruni-and-at-itakaon-the-lower-essequibo-these-have-the-following-structures-the-rock-is-made-up-of-a-micromosaic-of-quartz-and-feldspar-someof-the-granules-of-the-latter-showing-the-characteristics-of-microclineand-others-of-o-image336913324.html.

 If you do not want to visit that page, you can return to the previous page.