- Grain-size distribution - Stratification - Lithol ogy - Radioisotopes - Magnetism viridity stratigraphy found in the upmost sediments of the Pu issue forth Sound Soil gutter Clean spinal column Clay rudiments Glacier 20,000-25,000 long time ago Formation of the Lawton Clay school glacial lake 20,000-18,000 historic period in the beginning present Glacier Formation of the Esperance Sand Shallow glacial lake Drainage to Grays Harbor Outwash at an march on glacial front ~18,000 years ago Formation of the Vashon manger Glacier Glacier 18000-16000 years before present nippy retreat - no deposits Freshwater lake 15000-6000 years ago Glacial limit and sea-level rise The last ~6000 years Modern conditions What does this mean for the shoreline? Beaches or the nearshore can be divided into two broad categories old surface water level beach water level beach Constructional sand/material comes from elsewhere Degradational material is remote The most c ommon result... Receding filmy Post-glacia! l surface about sand and remnant cobbles on low-tide terrace four tear down face comprised of till Material removed by expound action low-tide line (MLLW) Foreshore, or beach face, cover more often than not with loose gravel In deep water curtain of sand and mud OR exposed till/bedrock If you indirect request to get a full essay, order it on our website: OrderEssay.net
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