![\"Four](\"https:\/\/rwu.pressbooks.pub\/app\/uploads\/sites\/7\/2017\/01\/figure13.1.2-1.png\")
<\/a> Figure 13.1.1<\/strong> Various beach substrates. Clockwise from top left: Punaluu Black Sand Beach, Hawaii, USA (Diego Delso [CC BY-SA 3.0], via Wikimedia Commons); Shell Beach, Shark Bay, Western Australia (Brian W. Schaller (Own work) [CC BY-NC-SA 3.0], via Wikimedia Commons); white coral sand beach in the Maldives (http:\/\/www.elitedivingagency.com\/, [CC BY-SA 3.0] via Wikimedia Commons); rocky beach at Killbear Provincial Park in Ontario, Canada (John Vetterli (originally posted to Flickr as Beach) [CC BY-SA 2.0], via Wikimedia Commons).[\/caption]The shoreline is divided up into multiple zones (Figure 13.1.2). The [pb_glossary id=\"558\"]backshore [\/pb_glossary]<\/strong> is the region of the beach above the high tide line, which is only submerged under unusually high wave conditions, such as during storms. The [pb_glossary id=\"758\"]foreshore [\/pb_glossary] <\/strong>lies between the high tide and low tide lines; it is submerged during high tide and is exposed during low tide. The [pb_glossary id=\"960\"]nearshore [\/pb_glossary]<\/strong> extends from the low tide line to the depth where wave action is no longer influenced by the bottom, i.e. to where the depth exceeds the [pb_glossary id=\"1248\"]wave base[\/pb_glossary] (section 10.1<\/a>).\u00a0 Finally, the [pb_glossary id=\"992\"]offshore [\/pb_glossary]<\/strong> zone represents the depths beyond the nearshore region.\r\n\r\nAlong the beach itself, the area above the high tide line is called the [pb_glossary id=\"586\"]berm[\/pb_glossary]<\/strong>, which is usually dry and relatively flat. The berm often ends with a berm crest or berm [pb_glossary id=\"1104\"]scarp[\/pb_glossary]<\/strong>, which is a steeper wall carved out by wave action that leads down to the foreshore. The foreshore has a number of other names, including the [pb_glossary id=\"1958\"]beach face[\/pb_glossary]<\/strong>, the [pb_glossary id=\"870\"]intertidal [\/pb_glossary]<\/strong> or [pb_glossary id=\"906\"]littoral zone[\/pb_glossary]<\/strong>, and if the area is fairly flat, the [pb_glossary id=\"916\"]low tide terrace[\/pb_glossary]<\/strong>. Just off shore from the beach there are often [pb_glossary id=\"910\"]longshore bars[\/pb_glossary]<\/strong> and longshore troughs running parallel to the beach. The longshore bars are accumulations of sand that are deposited by wave action and [pb_glossary id=\"912\"]longshore currents[\/pb_glossary] (section 13.2<\/a>). The decrease in depth above longshore bars is what often causes waves to start to break well before reaching the beach (section 10.3<\/a>).\r\n\r\n \r\n\r\n[caption id=\"attachment_450\" align=\"aligncenter\" width=\"1024\"]<\/a> Figure 13.1.2<\/strong> The zones of a typical beach (Modified by PW from Steven Earle, \"Physical Geology\").[\/caption]\r\n\r\nThe sand or other particles that make up the beach are distributed by wave action. The water that moves over a beach through incoming waves is called [pb_glossary id=\"1200\"]swash[\/pb_glossary]<\/strong>, and it also contains suspended sand grains that can get deposited on the beach. Some of the swash percolates into the sand while the rest of the water washes back out as [pb_glossary id=\"560\"]backwash [\/pb_glossary] <\/strong>as the wave recedes. Backwash removes sand from the beach and returns it to the ocean. Sand will therefore be deposited or eroded depending on which process is dominant. If wave action is light, a lot of incoming water gets absorbed by the sand, so swash dominates. Under heavier waves the beach becomes saturated with water, so less can be absorbed, and backwash is dominant. This leads to seasonal cycles in beach structure; waves are heavier during the winter as a result of stormier conditions at sea, so backwash dominates and sand is removed from the beach and deposited offshore in [pb_glossary id=\"910\"]longshore bars[\/pb_glossary]. In the summer the waves are gentler, swash dominates, and the sand is transported from the longshore bar and deposited on the shore to create a wider, sandy beach (Figure 13.1.3).\r\n\r\n \r\n\r\n[caption id=\"attachment_451\" align=\"aligncenter\" width=\"600\"]<\/a> Figure 13.1.3<\/strong> The differences between summer and winter on beaches in areas where the winter conditions are rougher and waves have a shorter wavelength but higher energy. In winter, sand from the beach is stored offshore (Steven Earle, \"Physical Geology\").[\/caption]\r\n\r\n ","rendered":"For most people, when they think of coastal areas they picture a beach, and the beach that they imagine is probably a typical sandy beach composed of quartz <\/a> sand grains (section 12.2<\/a>). But beaches are comprised of whatever types of sediments <\/a> are dominant in the local area. For example, parts of Hawaii and Iceland are famous for their black sand beaches, made up of eroded basalt <\/a> and other volcanic materials. The beautiful tropical white sand beaches we see in travel ads are largely composed of the crushed calcium carbonate remains of coral skeletons (much of which has been chewed up and excreted by a fish before we happily run our toes through it!)\u00a0 Other beaches may lack sand altogether and instead be dominated by small shells, or larger rocks or pebbles (Figure 13.1.1).<\/p>\n <\/p>\n The shoreline is divided up into multiple zones (Figure 13.1.2). The backshore <\/a><\/strong> is the region of the beach above the high tide line, which is only submerged under unusually high wave conditions, such as during storms. The foreshore <\/a> <\/strong>lies between the high tide and low tide lines; it is submerged during high tide and is exposed during low tide. The nearshore <\/a><\/strong> extends from the low tide line to the depth where wave action is no longer influenced by the bottom, i.e. to where the depth exceeds the wave base<\/a> (section 10.1<\/a>).\u00a0 Finally, the offshore <\/a><\/strong> zone represents the depths beyond the nearshore region.<\/p>\n Along the beach itself, the area above the high tide line is called the berm<\/a><\/strong>, which is usually dry and relatively flat. The berm often ends with a berm crest or berm scarp<\/a><\/strong>, which is a steeper wall carved out by wave action that leads down to the foreshore. The foreshore has a number of other names, including the beach face<\/strong>, the intertidal <\/a><\/strong> or littoral zone<\/a><\/strong>, and if the area is fairly flat, the low tide terrace<\/a><\/strong>. Just off shore from the beach there are often longshore bars<\/a><\/strong> and longshore troughs running parallel to the beach. The longshore bars are accumulations of sand that are deposited by wave action and longshore currents<\/a> (section 13.2<\/a>). The decrease in depth above longshore bars is what often causes waves to start to break well before reaching the beach (section 10.3<\/a>).<\/p>\n <\/p>\n The sand or other particles that make up the beach are distributed by wave action. The water that moves over a beach through incoming waves is called swash<\/a><\/strong>, and it also contains suspended sand grains that can get deposited on the beach. Some of the swash percolates into the sand while the rest of the water washes back out as backwash <\/a> <\/strong>as the wave recedes. Backwash removes sand from the beach and returns it to the ocean. Sand will therefore be deposited or eroded depending on which process is dominant. If wave action is light, a lot of incoming water gets absorbed by the sand, so swash dominates. Under heavier waves the beach becomes saturated with water, so less can be absorbed, and backwash is dominant. This leads to seasonal cycles in beach structure; waves are heavier during the winter as a result of stormier conditions at sea, so backwash dominates and sand is removed from the beach and deposited offshore in longshore bars<\/a>. In the summer the waves are gentler, swash dominates, and the sand is transported from the longshore bar and deposited on the shore to create a wider, sandy beach (Figure 13.1.3).<\/p>\n<\/a><\/a>