From d7f4c5333a25394974f4935db5c81bd580abb580 Mon Sep 17 00:00:00 2001 From: Koukofikis <athanasios.koukofikis@hft-stuttgart.de> Date: Wed, 5 May 2021 10:41:37 +0000 Subject: [PATCH] Update index.html --- public/home/index.html | 12 +----------- 1 file changed, 1 insertion(+), 11 deletions(-) diff --git a/public/home/index.html b/public/home/index.html index efff155..acd6ebc 100644 --- a/public/home/index.html +++ b/public/home/index.html @@ -59,17 +59,7 @@ <h1>Abstract</h1> <p> - Lorem ipsum dolor sit amet, consectetur adipiscing elit. Quisque pellentesque diam ipsum, nec - ultricies sem mollis et. Phasellus porttitor nec felis quis ultricies. In venenatis faucibus nisl - sed facilisis. Cras sapien nibh, dignissim at eros quis, commodo lobortis eros. Sed a massa - eleifend, dictum elit at, blandit magna. Nullam auctor enim nec orci luctus sagittis. Nunc blandit - quam nec laoreet egestas. Nulla feugiat nisl lacus, a viverra nisi hendrerit vitae. In nibh arcu, - sodales in enim tincidunt, tempus imperdiet ex. Aliquam fermentum augue magna, vel accumsan augue - consequat et. Vestibulum id interdum orci, a aliquam sapien. Vivamus eu ipsum sollicitudin, aliquet - arcu ut, ornare massa. Suspendisse tincidunt lectus a odio ultrices interdum. Praesent vitae sodales - urna, vitae sagittis ex. Vivamus tincidunt nisi ultrices lectus dapibus, at placerat nisl elementum. - Fusce cursus, sapien in tincidunt pellentesque, mi erat mollis nibh, ut maximus tortor magna vitae - nibh. + Since they are still preserved in the rocks for us to see, they must have been formed quite recently, that is, geologically speaking. What can explain these striations and their common orientation? Did you ever hear about the Great Ice Age or the Pleistocene Epoch? Less than one million years ago, in fact, some 12,000 years ago, an ice sheet many thousands of feet thick rode over Burke Mountain in a southeastward direction. The many boulders frozen to the underside of the ice sheet tended to scratch the rocks over which they rode. The scratches or striations seen in the park rocks were caused by these attached boulders. The ice sheet also plucked and rounded Burke Mountain into the shape it possesses today. </p> </div> -- GitLab