Depositionjg
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The document defines and describes various types of geological deposits and depositions. It explains that a beach is a deposit of sand next to a body of water. A sand dune is a mound of sand deposited by wind. Loess is a deposit made of fine layers of glacial silt and sand deposited by wind. A moraine is a ridge of till deposited at the edge of a glacier. A sandbar is a long ridge of sand in a river or near a shore. A talus slope is a cone-shaped deposit at the bottom of a hill caused by gravity. A delta is a finger-shaped deposit of sediments at the mouth of a river. A levee is a ridge-like deposit of sediments on
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Coastal features of erosion
This is an interactive power point that helps students discoverer the processes that shape our coastal land forms.
Spit, bar or tombolo
Beaches form in sheltered environments like bays through the processes of deposition. Spits are formed when longshore drift causes sediment to accumulate into narrow extensions of land along a shoreline. Bars are similar to spits but connect two areas of mainland, while tombolos connect an island to the mainland through a double-barred spit formation.
Transportation Deposition
Beaches form through the process of erosion and deposition by ocean waves. Sediment such as sand and pebbles is eroded from cliffs and shores by wave action and transported down the coast by longshore drift. This sediment is eventually deposited and builds up over time to create beaches. The size and shape of beaches depends on the type of sediment - shingle beaches are steeper while sand beaches have a more gentle slope. Features like spits, bars, and tombolos are also formed through deposition when sediment carried by longshore drift accumulates in different ways.
5. landforms created by coastal deposition
Beaches, spits, and bars are landforms created by coastal depositional processes. Beaches form along shorelines through the deposition of sediment by wave action. As sediment is transported along the shoreline by longshore drift, it can build up into narrow peninsulas called spits. Spits often form at the mouths of estuaries, where the changing direction of the coastline causes sediment to deposit. Bars may develop offshore or near the mouths of rivers, made of sediment that has been deposited and built up over time.
Longshore drift and spit formation
This lesson teaches about landforms created by longshore drift, including bars, spits, and tombolos. By the end of the lesson, students will be able to name 3 depositional landforms, describe the process of longshore drift, and explain how it forms bars, spits, and tombolos. The lesson will include diagrams demonstrating longshore drift and how spits are formed through the movement of sediment along a coastline.
Headlands
The document discusses various coastal landforms created by erosion processes along the coastline. It focuses on the specific example of Old Harry Rocks, located on the Dorset coast in England. Old Harry Rocks consists of two chalk stacks that were formed as the surrounding softer clay was eroded away by waves and other processes over centuries. Hydraulic action, corrosion and abrasion helped erode weaknesses in the chalk cliff and form caves, arches and eventually the remaining stacks that make up Old Harry Rocks today. One of the stacks used to be part of an arch but collapsed, becoming a stump. The document analyzes how these specific landforms were formed through coastal erosion.
Beach Profiles
Beaches have three main components - the nearshore, foreshore, and backshore. The nearshore extends seaward of the shoreline and contains sand bars formed by sediment deposition as wave energy is lost. The foreshore is the area between low and high tide marks affected daily by swash and backwash, depositing and returning sediment. The backshore lies beyond the foreshore and contains dunes, with sediment transported there during storms. Key beach features include berms, ridges and runnels, cusps, spits, and bars, formed by processes like deposition, swash action, and longshore drift.
Spits
A spit is a landform created by the deposition of sediment transported by longshore drift. Sediment is carried along the coast until the direction changes, causing deposition and the formation of a curved spit. Over time, the deposited sediment builds up in layers from mudflats to salt marsh and eventually freshwater marsh. As wind directions change, the end of the spit may curve further, forming hooked shapes. Spits can grow across river mouths or bays, diverting rivers or connecting islands to mainland via tombolos.
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Coastal features of erosion
This is an interactive power point that helps students discoverer the processes that shape our coastal land forms.
Spit, bar or tombolo
Beaches form in sheltered environments like bays through the processes of deposition. Spits are formed when longshore drift causes sediment to accumulate into narrow extensions of land along a shoreline. Bars are similar to spits but connect two areas of mainland, while tombolos connect an island to the mainland through a double-barred spit formation.
Transportation Deposition
Beaches form through the process of erosion and deposition by ocean waves. Sediment such as sand and pebbles is eroded from cliffs and shores by wave action and transported down the coast by longshore drift. This sediment is eventually deposited and builds up over time to create beaches. The size and shape of beaches depends on the type of sediment - shingle beaches are steeper while sand beaches have a more gentle slope. Features like spits, bars, and tombolos are also formed through deposition when sediment carried by longshore drift accumulates in different ways.
5. landforms created by coastal deposition
Beaches, spits, and bars are landforms created by coastal depositional processes. Beaches form along shorelines through the deposition of sediment by wave action. As sediment is transported along the shoreline by longshore drift, it can build up into narrow peninsulas called spits. Spits often form at the mouths of estuaries, where the changing direction of the coastline causes sediment to deposit. Bars may develop offshore or near the mouths of rivers, made of sediment that has been deposited and built up over time.
Longshore drift and spit formation
This lesson teaches about landforms created by longshore drift, including bars, spits, and tombolos. By the end of the lesson, students will be able to name 3 depositional landforms, describe the process of longshore drift, and explain how it forms bars, spits, and tombolos. The lesson will include diagrams demonstrating longshore drift and how spits are formed through the movement of sediment along a coastline.
Headlands
The document discusses various coastal landforms created by erosion processes along the coastline. It focuses on the specific example of Old Harry Rocks, located on the Dorset coast in England. Old Harry Rocks consists of two chalk stacks that were formed as the surrounding softer clay was eroded away by waves and other processes over centuries. Hydraulic action, corrosion and abrasion helped erode weaknesses in the chalk cliff and form caves, arches and eventually the remaining stacks that make up Old Harry Rocks today. One of the stacks used to be part of an arch but collapsed, becoming a stump. The document analyzes how these specific landforms were formed through coastal erosion.
Beach Profiles
Beaches have three main components - the nearshore, foreshore, and backshore. The nearshore extends seaward of the shoreline and contains sand bars formed by sediment deposition as wave energy is lost. The foreshore is the area between low and high tide marks affected daily by swash and backwash, depositing and returning sediment. The backshore lies beyond the foreshore and contains dunes, with sediment transported there during storms. Key beach features include berms, ridges and runnels, cusps, spits, and bars, formed by processes like deposition, swash action, and longshore drift.
Spits
A spit is a landform created by the deposition of sediment transported by longshore drift. Sediment is carried along the coast until the direction changes, causing deposition and the formation of a curved spit. Over time, the deposited sediment builds up in layers from mudflats to salt marsh and eventually freshwater marsh. As wind directions change, the end of the spit may curve further, forming hooked shapes. Spits can grow across river mouths or bays, diverting rivers or connecting islands to mainland via tombolos.
Formation Of A Spit James Benson
A spit is formed through the process of longshore drift. As waves approach the shore at an angle, sediment is carried along the coast until it reaches a change in direction, such as a headland. The sediment builds up over time to form a sandbar that stretches out into the sea. Spits continue growing until reaching an area of fast water flow or change in wind direction. Sheltered water and salt marshes form behind the spit, providing habitat for wildlife.
Formation of spits, tombolos and bars
Spits, tombolos, and bars are coastal landforms created by the deposition of material through longshore drift. Spits project from the coastline into the sea, tombolos join mainland to islands, and bars connect two headlands and cut off a bay. They form in areas of reduced wave energy where deposited material builds up over time through the processes of longshore drift and deposition.
L3.ap longshore drift and deposition
The document summarizes various coastal erosion processes that shape coastlines:
1) Attrition occurs as waves carry rocks that knock against each other, breaking them down into smaller pieces over time.
2) Abrasion involves the dissolving of limestone by carbonic acid in seawater and the expansion of salt crystals in the rock causing it to disintegrate.
3) Hydraulic action is the wearing away of cliffs by sand, shingle and boulders hurled against them powerfully by wave action.
Headlands and Bays
The document discusses different types of weathering and erosion processes that shape coastlines. Waves erode softer rock faster than harder rock, forming bays surrounded by harder headlands that are more resistant to erosion. Deposition occurs in the sheltered bays, creating beaches, while the exposed headlands continue to be eroded by waves. Biological, chemical, freeze-thaw and other processes also contribute to coastal weathering and erosion over time.
Coasts: Headlands and Bays
This document provides information about headlands and bays, including:
1) Headlands and bays are formed by the uneven erosion of coastlines composed of bands of rock with varying resistance. More resistant rocks like granite and basalt form headlands, while less resistant rocks like chalk, sandstone and shale erode more quickly to form bays.
2) Waves concentrate their energy at headlands, eroding them more, while weakening along wider bays where sediments are deposited.
3) Students are expected to learn about beaches, spits and tombolos from their textbook for homework, with examples of different beach gradients based on sediment coarseness.
Beaches AS
Beaches are depositional landforms that form along coastlines where sand and shingle accumulate faster than they are removed by waves. Beaches represent accumulated material deposited between low and high tides. Beach material comes from cliff erosion, offshore sources, and rivers. Sand produces gently sloped beaches below 5 degrees, while shingle produces steeper beaches from 10-20 degrees. Factors like wave energy, type, and longshore drift influence beach profiles.
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This document provides an overview of coasts and coastal processes. It begins with an introduction to the topics that will be covered, including the syllabus, case studies, coastal processes, and exam technique. Case studies include the Holderness Coast, Flamborough Head, and Spurn Point. Coastal processes such as hydraulic action, abrasion, attrition, and solution are explained. Exam advice is given around answering 6-marker questions by explaining coastal landforms and processes in a structured sequence.
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Coastal erosion creates several landforms along shorelines including cliffs, headlands, bays, caves, arches, and stacks. The type of landform created depends on factors like the underlying rock material, with hard rocks like basalt resisting erosion to form steep cliffs and headlands, while softer rocks erode more quickly to form gently sloping cliffs. Cliff erosion occurs through both marine processes like waves and subaerial processes like weathering, and the rate and shape of the cliff changes over time in an episodic cycle as material accumulates and is removed from the cliff base.
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The document discusses different types of coastal landforms formed by erosion and deposition. It describes four types of sediment transportation along coasts: dissolution, suspension, saltation, and traction. It also discusses the formation of headlands and bays due to differences in the resistance of the underlying rock. When waves have low energy and conditions are calm, deposition occurs, forming landforms like beaches, spits, tombolos, sand bars and barrier islands.
Sediment Cells And Sources
This document discusses sediment cells and sources along coastlines. It defines sediment cells as discrete areas where sediment movement is largely self-contained. Sediment can come from erosion of cliffs, sea beds, and rivers being transported by waves, currents, tides and wind. Sediment is either stored in depositional landforms like beaches or transported through the cell. The UK has 11 major sediment cells that operate in a state of dynamic equilibrium. Coastal processes like hydraulic action, abrasion, attrition, and corrosion cause different rates and types of erosion along coastlines. Mass movement processes also influence erosion, including soil creep, solifluction, and mudflows.
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Spits and bars are depositional coastal landforms formed by processes such as longshore drift. A spit is a depositional landform that extends from the shore out to sea, often curved in shape due to opposing winds and currents. A bar occurs where a spit grows across a bay, enclosing the bay to form a lagoon, or forms offshore due to breaking waves. Longshore drift transports sediment along the coast and causes deposition of material in certain areas, gradually building up spits and bars.
Tombolo
Tombolos are ridges of sand or pebbles that connect islands to the mainland. They are formed over time by longshore drift, which is the movement of beach materials like sand and pebbles along the coastline. When the direction of the coastline changes, beach materials continue to be transported in their original direction and build up underwater to create spits. As spits grow larger, they can eventually connect to nearby islands, forming tombolos like Chesil Beach, an 18-mile-long ridge of pebbles in the UK.
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The five main river processes that shape the river landscape are erosion, transportation, deposition, mass movement, and weathering. Erosion processes include hydraulic action from water force, abrasion from rocks hitting the river bed, solution where rocks dissolve in water, and attrition where rocks wear down from bumping together. Transportation involves traction moving large rocks along the river bed, saltation bouncing small sediment particles, and suspension carrying very fine particles in the water. Deposition occurs when the river drops its sediment load due to decreasing velocity or volume. Mass movement comprises soil creep on slopes, landslides from undercutting, and debris flows like liquid down hills. Weathering includes mechanical, chemical, and biological processes breaking down rock and sediment.
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This document discusses river landforms in the upper course of a river. It begins by explaining that river landforms are shaped by the geology of an area and river processes. The dominant process in the upper course is erosion, which cuts down vertically to form a V-shaped valley. One landform discussed is interlocking spurs, which are areas of resistant rock that the river bends and winds around, leaving protruding areas of hard rock between indentations eroded into softer rock. Another landform is waterfalls and gorges, which form where there are bands of hard and soft rock. Waterfalls erode upstream over time, deepening plunge pools and forming steep rock walls of a gorge as the waterfall retreats
L4 ap middle and lower course features
The document describes landforms created by erosion and deposition in the middle and lower courses of a river. In the middle course, meanders and oxbow lakes are formed. Meanders create point bars on the inside bend through deposition and river cliffs on the outside through erosion. Over time, meander necks may be cut off, forming oxbow lakes. In the lower course, levees and floodplains are formed. Levees are deposited along river banks during flooding, while floodplains are wide, flat areas deposited during over-bank flooding events.
Depositional landforms
This document summarizes several types of depositional landforms formed by coastal processes. It describes spits as narrow accumulations of sand or gravel extending into the sea from the coastline. As sediment is deposited, spits can grow into barrier beaches, barrier islands, or tombolos connecting an island to the mainland. It also discusses how wave refraction around headlands and islands leads to erosion on headlands and deposition in sheltered bays, forming features like bayhead beaches.
Coastal Processes on the Holderness Coast
1) The UK coastline has been divided into coastal cells and sub-cells to simplify understanding coastal processes. The East Riding coastline is designated as sub-cell 2a.
2) Cliff erosion along the East Riding coast is complex and dynamic, driven by random wave and tidal forces. Erosion produces sediment that is sorted and transported south by these coastal processes. Beach levels fluctuate in response, impacting erosion rates.
3) Erosion occurs in four zones - the cliff face, nearshore beach, offshore clay face, and protected offshore seabed. Cliff erosion averages 1.7m/year while offshore erosion likely matches this rate, totaling around 3 million cubic meters of erosion
Sec3 Coast features
The document discusses various coastal landforms formed by erosion and deposition processes along shorelines. It describes how cliffs and wave-cut platforms form through wave erosion and undercutting of rock faces. It also explains how alternating hard and soft rock layers lead to the development of headlands and bays, and how wave refraction directs more energy towards headlands. Finally, it outlines how beaches, spits, and tombolos are depositional landforms that form through transport and accumulation of sediments by waves and currents.
Coastal Landforms
The document discusses various coastal landforms created by erosion and deposition processes along shorelines. It describes landforms such as headlands and bays, cliffs and wave-cut platforms, caves, arches, stacks, and stumps which are formed by coastal erosion. Beaches and spits are landforms created by coastal deposition, with beaches forming in sheltered areas between high and low tide lines, and spits forming as narrow ridges projecting from the coast due to longshore drift depositing materials.
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The document outlines the topics and objectives for a lesson on coastal landforms and processes. It includes sections on agents shaping coasts like waves, tides, and currents; coastal processes; coastal landforms; coastal protection measures; and diagrams and videos illustrating concepts. The lesson will describe factors affecting wave energy, types of wave movement including swash and backwash, and different types of constructive and destructive waves.
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Earthquakes occur when stress builds up in the Earth's crust and causes rock to break along faults. There are three main types of faults - strike-slip faults, where rock slides past each other; normal faults, where one side drops down; and reverse faults, where one side is pushed up. Seismic waves called P waves and S waves travel out from the earthquake focus and can be measured with seismographs. The intensity and magnitude of earthquakes are measured using scales like the Mercalli and Moment Magnitude scales.
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Formation Of A Spit James Benson
A spit is formed through the process of longshore drift. As waves approach the shore at an angle, sediment is carried along the coast until it reaches a change in direction, such as a headland. The sediment builds up over time to form a sandbar that stretches out into the sea. Spits continue growing until reaching an area of fast water flow or change in wind direction. Sheltered water and salt marshes form behind the spit, providing habitat for wildlife.
Formation of spits, tombolos and bars
Spits, tombolos, and bars are coastal landforms created by the deposition of material through longshore drift. Spits project from the coastline into the sea, tombolos join mainland to islands, and bars connect two headlands and cut off a bay. They form in areas of reduced wave energy where deposited material builds up over time through the processes of longshore drift and deposition.
L3.ap longshore drift and deposition
The document summarizes various coastal erosion processes that shape coastlines:
1) Attrition occurs as waves carry rocks that knock against each other, breaking them down into smaller pieces over time.
2) Abrasion involves the dissolving of limestone by carbonic acid in seawater and the expansion of salt crystals in the rock causing it to disintegrate.
3) Hydraulic action is the wearing away of cliffs by sand, shingle and boulders hurled against them powerfully by wave action.
Headlands and Bays
The document discusses different types of weathering and erosion processes that shape coastlines. Waves erode softer rock faster than harder rock, forming bays surrounded by harder headlands that are more resistant to erosion. Deposition occurs in the sheltered bays, creating beaches, while the exposed headlands continue to be eroded by waves. Biological, chemical, freeze-thaw and other processes also contribute to coastal weathering and erosion over time.
Coasts: Headlands and Bays
This document provides information about headlands and bays, including:
1) Headlands and bays are formed by the uneven erosion of coastlines composed of bands of rock with varying resistance. More resistant rocks like granite and basalt form headlands, while less resistant rocks like chalk, sandstone and shale erode more quickly to form bays.
2) Waves concentrate their energy at headlands, eroding them more, while weakening along wider bays where sediments are deposited.
3) Students are expected to learn about beaches, spits and tombolos from their textbook for homework, with examples of different beach gradients based on sediment coarseness.
Beaches AS
Beaches are depositional landforms that form along coastlines where sand and shingle accumulate faster than they are removed by waves. Beaches represent accumulated material deposited between low and high tides. Beach material comes from cliff erosion, offshore sources, and rivers. Sand produces gently sloped beaches below 5 degrees, while shingle produces steeper beaches from 10-20 degrees. Factors like wave energy, type, and longshore drift influence beach profiles.
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This document provides an overview of coasts and coastal processes. It begins with an introduction to the topics that will be covered, including the syllabus, case studies, coastal processes, and exam technique. Case studies include the Holderness Coast, Flamborough Head, and Spurn Point. Coastal processes such as hydraulic action, abrasion, attrition, and solution are explained. Exam advice is given around answering 6-marker questions by explaining coastal landforms and processes in a structured sequence.
Coastal Features Created By Erosion Sherry
Coastal erosion creates several landforms along shorelines including cliffs, headlands, bays, caves, arches, and stacks. The type of landform created depends on factors like the underlying rock material, with hard rocks like basalt resisting erosion to form steep cliffs and headlands, while softer rocks erode more quickly to form gently sloping cliffs. Cliff erosion occurs through both marine processes like waves and subaerial processes like weathering, and the rate and shape of the cliff changes over time in an episodic cycle as material accumulates and is removed from the cliff base.
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The document discusses different types of coastal landforms formed by erosion and deposition. It describes four types of sediment transportation along coasts: dissolution, suspension, saltation, and traction. It also discusses the formation of headlands and bays due to differences in the resistance of the underlying rock. When waves have low energy and conditions are calm, deposition occurs, forming landforms like beaches, spits, tombolos, sand bars and barrier islands.
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This document discusses sediment cells and sources along coastlines. It defines sediment cells as discrete areas where sediment movement is largely self-contained. Sediment can come from erosion of cliffs, sea beds, and rivers being transported by waves, currents, tides and wind. Sediment is either stored in depositional landforms like beaches or transported through the cell. The UK has 11 major sediment cells that operate in a state of dynamic equilibrium. Coastal processes like hydraulic action, abrasion, attrition, and corrosion cause different rates and types of erosion along coastlines. Mass movement processes also influence erosion, including soil creep, solifluction, and mudflows.
8. spits and bars
Spits and bars are depositional coastal landforms formed by processes such as longshore drift. A spit is a depositional landform that extends from the shore out to sea, often curved in shape due to opposing winds and currents. A bar occurs where a spit grows across a bay, enclosing the bay to form a lagoon, or forms offshore due to breaking waves. Longshore drift transports sediment along the coast and causes deposition of material in certain areas, gradually building up spits and bars.
Tombolo
Tombolos are ridges of sand or pebbles that connect islands to the mainland. They are formed over time by longshore drift, which is the movement of beach materials like sand and pebbles along the coastline. When the direction of the coastline changes, beach materials continue to be transported in their original direction and build up underwater to create spits. As spits grow larger, they can eventually connect to nearby islands, forming tombolos like Chesil Beach, an 18-mile-long ridge of pebbles in the UK.
L1 ap drainage basin and river processes
The five main river processes that shape the river landscape are erosion, transportation, deposition, mass movement, and weathering. Erosion processes include hydraulic action from water force, abrasion from rocks hitting the river bed, solution where rocks dissolve in water, and attrition where rocks wear down from bumping together. Transportation involves traction moving large rocks along the river bed, saltation bouncing small sediment particles, and suspension carrying very fine particles in the water. Deposition occurs when the river drops its sediment load due to decreasing velocity or volume. Mass movement comprises soil creep on slopes, landslides from undercutting, and debris flows like liquid down hills. Weathering includes mechanical, chemical, and biological processes breaking down rock and sediment.
L3 ap upper course features
This document discusses river landforms in the upper course of a river. It begins by explaining that river landforms are shaped by the geology of an area and river processes. The dominant process in the upper course is erosion, which cuts down vertically to form a V-shaped valley. One landform discussed is interlocking spurs, which are areas of resistant rock that the river bends and winds around, leaving protruding areas of hard rock between indentations eroded into softer rock. Another landform is waterfalls and gorges, which form where there are bands of hard and soft rock. Waterfalls erode upstream over time, deepening plunge pools and forming steep rock walls of a gorge as the waterfall retreats
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The document describes landforms created by erosion and deposition in the middle and lower courses of a river. In the middle course, meanders and oxbow lakes are formed. Meanders create point bars on the inside bend through deposition and river cliffs on the outside through erosion. Over time, meander necks may be cut off, forming oxbow lakes. In the lower course, levees and floodplains are formed. Levees are deposited along river banks during flooding, while floodplains are wide, flat areas deposited during over-bank flooding events.
Depositional landforms
This document summarizes several types of depositional landforms formed by coastal processes. It describes spits as narrow accumulations of sand or gravel extending into the sea from the coastline. As sediment is deposited, spits can grow into barrier beaches, barrier islands, or tombolos connecting an island to the mainland. It also discusses how wave refraction around headlands and islands leads to erosion on headlands and deposition in sheltered bays, forming features like bayhead beaches.
Coastal Processes on the Holderness Coast
1) The UK coastline has been divided into coastal cells and sub-cells to simplify understanding coastal processes. The East Riding coastline is designated as sub-cell 2a.
2) Cliff erosion along the East Riding coast is complex and dynamic, driven by random wave and tidal forces. Erosion produces sediment that is sorted and transported south by these coastal processes. Beach levels fluctuate in response, impacting erosion rates.
3) Erosion occurs in four zones - the cliff face, nearshore beach, offshore clay face, and protected offshore seabed. Cliff erosion averages 1.7m/year while offshore erosion likely matches this rate, totaling around 3 million cubic meters of erosion
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The document discusses various coastal landforms formed by erosion and deposition processes along shorelines. It describes how cliffs and wave-cut platforms form through wave erosion and undercutting of rock faces. It also explains how alternating hard and soft rock layers lead to the development of headlands and bays, and how wave refraction directs more energy towards headlands. Finally, it outlines how beaches, spits, and tombolos are depositional landforms that form through transport and accumulation of sediments by waves and currents.
Coastal Landforms
The document discusses various coastal landforms created by erosion and deposition processes along shorelines. It describes landforms such as headlands and bays, cliffs and wave-cut platforms, caves, arches, stacks, and stumps which are formed by coastal erosion. Beaches and spits are landforms created by coastal deposition, with beaches forming in sheltered areas between high and low tide lines, and spits forming as narrow ridges projecting from the coast due to longshore drift depositing materials.
Coasts 1 blog
The document outlines the topics and objectives for a lesson on coastal landforms and processes. It includes sections on agents shaping coasts like waves, tides, and currents; coastal processes; coastal landforms; coastal protection measures; and diagrams and videos illustrating concepts. The lesson will describe factors affecting wave energy, types of wave movement including swash and backwash, and different types of constructive and destructive waves.
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- 10. 5. What is this deposition?
- 12. 6. What is this deposition?
- 14. 7. What is this deposition?
- 16. 8. What is this deposition?
- 18. 9. What is this deposition?
- 20. 10. What is this general category of deposition called?
- 22. 11. What is this general category of deposition called?
- 24. 13. What is this deposition?
- 29. **Identify this deposit. D.
- 30. **Identify this deposit. E.
- 31. The End F. What is this deposition? © Copyright 2004 - 2005. M. J. Krech. All rights reserved.