Field assignment part 2
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This document summarizes examples of different geological features and processes observed in Virginia Beach, Virginia through photographs. Examples include chemical weathering on a headstone and manhole cover, a house destroyed by ground subsidence from mass wasting, continental and marine sedimentary environments at a lake and oceanfront, and practical uses like a stormwater pond and the Chesapeake Bay Bridge Tunnel infrastructure. The author was unable to find a local example of a fault to include.
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The coast line is under threat from hydraulic action and corrosion which is undercutting the cliffs and forming arch caves as rocks are thrown into the cliff by waves. A spit was formed by longshore drift where prevailing winds blow beach material down the coast to form a spit.
The sea
The sea constantly changes coastlines through erosion, transportation, and deposition of material. Waves erode the coastline through processes like hydraulic action and abrasion, forming landforms such as cliffs, bays, and sea caves. Material is transported along the shore by swash and backwash and through longshore drift. Deposition by the sea creates beaches, sand dunes, sand spits, and lagoons. People build structures like sea walls, place boulders, and construct groynes to protect coastlines from erosion while also utilizing coastlines for tourism, industry, and recreation.
Waves
Strong waves erode and deposit material on shorelines over time, forming various landforms. This includes sea cliffs from cracks in rocks that widen and break off, sea caves carved out of weak rocks, sea arches formed when erosion joins cracks close together, and stacks remaining after arch roofs collapse. Beaches are also formed as waves temporarily deposit sand and soil.
Tectonics
The document discusses the structure and composition of the Earth. It is divided into sections on:
1) A comparison of the Earth's structure to a scotch egg, with the crust as the breadcrumbs, mantle as the meat, outer core as the egg white, and inner core as the yolk.
2) Plate tectonics and the distribution of earthquakes and volcanoes along plate boundaries.
3) The differences between oceanic and continental crust.
4) Types of plate boundaries including divergent, convergent, and conservative, and examples of each.
Coastal processes
Coastal systems can be divided into erosional shorelines and depositional shorelines based on dominant long-term processes. Erosional shorelines are dominated by erosive forces and typically have high-relief rocky coasts, while depositional shorelines are dominated by depositional processes and include environments like deltas, barrier islands, and reef coasts. Coasts experience various erosive and depositional processes from waves, such as refraction, longshore drift, and swash/backwash, which shape the shoreline over time. Stabilizing eroding coasts involves hard structures, beach nourishment, or relocation, but these approaches have limitations and tradeoffs.
Coastal and sea erosion
Coastal erosion is the wearing away of land and the displacement of the shoreline caused by natural forces like waves, winds, and tides. It can also be exacerbated by human activities. The document outlines various natural causes of coastal erosion like wave action, winds, tides, storms, and sea level rise, as well as human causes like construction and dredging. Factors that influence erosion rates include sediment sources and sinks, changes in sea level, and coastal geomorphology. Coastal erosion shapes coastlines slowly over time but can also occur catastrophically during storms or tsunamis.
Coastal erosion processes
This document discusses coastal studies and processes. It describes the different types of waves that impact coasts, including constructive waves that have weaker backwash and destructive waves that strongly erode coasts. The key coastal processes are erosion, transportation, and deposition. Erosional processes include corrasion, attrition, solution, and hydraulic action, which can be remembered with the acronym CASH. Factors influencing the rate of coastal erosion are the type of waves, the nature of coastal rocks, the gradient of the coast, and human activities.
Coastal processes
Slides on Coastal erosion, deposition and transport for Leaving Certificate Geography (Irish education system)
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The coast line is under threat from hydraulic action and corrosion which is undercutting the cliffs and forming arch caves as rocks are thrown into the cliff by waves. A spit was formed by longshore drift where prevailing winds blow beach material down the coast to form a spit.
The sea
The sea constantly changes coastlines through erosion, transportation, and deposition of material. Waves erode the coastline through processes like hydraulic action and abrasion, forming landforms such as cliffs, bays, and sea caves. Material is transported along the shore by swash and backwash and through longshore drift. Deposition by the sea creates beaches, sand dunes, sand spits, and lagoons. People build structures like sea walls, place boulders, and construct groynes to protect coastlines from erosion while also utilizing coastlines for tourism, industry, and recreation.
Waves
Strong waves erode and deposit material on shorelines over time, forming various landforms. This includes sea cliffs from cracks in rocks that widen and break off, sea caves carved out of weak rocks, sea arches formed when erosion joins cracks close together, and stacks remaining after arch roofs collapse. Beaches are also formed as waves temporarily deposit sand and soil.
Tectonics
The document discusses the structure and composition of the Earth. It is divided into sections on:
1) A comparison of the Earth's structure to a scotch egg, with the crust as the breadcrumbs, mantle as the meat, outer core as the egg white, and inner core as the yolk.
2) Plate tectonics and the distribution of earthquakes and volcanoes along plate boundaries.
3) The differences between oceanic and continental crust.
4) Types of plate boundaries including divergent, convergent, and conservative, and examples of each.
Coastal processes
Coastal systems can be divided into erosional shorelines and depositional shorelines based on dominant long-term processes. Erosional shorelines are dominated by erosive forces and typically have high-relief rocky coasts, while depositional shorelines are dominated by depositional processes and include environments like deltas, barrier islands, and reef coasts. Coasts experience various erosive and depositional processes from waves, such as refraction, longshore drift, and swash/backwash, which shape the shoreline over time. Stabilizing eroding coasts involves hard structures, beach nourishment, or relocation, but these approaches have limitations and tradeoffs.
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Coastal erosion is the wearing away of land and the displacement of the shoreline caused by natural forces like waves, winds, and tides. It can also be exacerbated by human activities. The document outlines various natural causes of coastal erosion like wave action, winds, tides, storms, and sea level rise, as well as human causes like construction and dredging. Factors that influence erosion rates include sediment sources and sinks, changes in sea level, and coastal geomorphology. Coastal erosion shapes coastlines slowly over time but can also occur catastrophically during storms or tsunamis.
Coastal erosion processes
This document discusses coastal studies and processes. It describes the different types of waves that impact coasts, including constructive waves that have weaker backwash and destructive waves that strongly erode coasts. The key coastal processes are erosion, transportation, and deposition. Erosional processes include corrasion, attrition, solution, and hydraulic action, which can be remembered with the acronym CASH. Factors influencing the rate of coastal erosion are the type of waves, the nature of coastal rocks, the gradient of the coast, and human activities.
Coastal processes
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land forms formed by seawaves
This document discusses erosional and depositional landforms caused by sea waves. It describes how sea waves erode coastal rocks through cracks and breaking pieces, forming sea cliffs, caves, arches and stacks. Sea caves are formed by wave erosion carving holes in the coastline. Arches are formed when sea caves on either side join together. Stacks remain when arch roofs collapse. Deposition by waves temporarily deposits sand and soil to form beaches. In conclusion, sea waves cause significant morphological changes along the shoreline through both erosional and depositional processes.
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Coastal landscapes
This document discusses various types of coastal erosion and protection methods. It describes the characteristics and impacts of constructive and destructive waves. It also explains various coastal landforms that form from erosion like cliffs, arches and stacks. Additionally, it outlines different coastal management techniques like riprap, seawalls, beach replenishment and managed retreat. The advantages and disadvantages of each protection strategy are provided.
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Waves are the primary force causing erosion along coastlines. Constructive waves build beaches up while destructive waves erode beaches. Coastal landforms like cliffs, caves, arches and stacks are formed through erosion processes. Longshore drift transports sediment along the coast, potentially building up spits or bars. The coast at Holderness, East Yorkshire is eroding rapidly, retreating over 1 meter per year due to its soft cliff material and destructive North Sea waves. Several villages have been lost and infrastructure like roads and gas facilities are threatened. Various coastal defenses have been installed with mixed success.
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4) Continental, marine, and transitional environments illustrated by photos of Sierra Nevada mountains, the Pacific Ocean, and Pismo Beach shoreline respectively.
Geology 1
The document discusses various geological features and concepts seen in photos taken around Pismo Beach, California and other locations. It includes photos of reverse and thrust faults seen in the shoreline of Pismo Beach. Other photos show mechanical weathering in an irrigation channel and a broken down street, erosion of a train, and a sedimentary environment at Pismo Beach shoreline transitioning from land to sea. The document also discusses sustainable practices at Simplot, a local chemical plant.
Geol3 presentation2 ( continued)
The document discusses different sedimentary environments and provides examples of each:
1) An example of erosion on a small scale showing harder surfaces preventing erosion underneath.
2) The marine environment being the continental shelf underwater, as seen in a photo of the Pacific Ocean.
3) A photo example of a continental environment with mountains collecting snow that melts into channels and deposits sediments downstream.
4) Transitional environments like coastlines and beaches seen in a photo of the author at a beach town as tides change the coastline exposure.
Part 2 rachel carter
This document summarizes several geological processes and environments observed by the author:
1) It describes frost wedging and oxidation seen in rocks near a creek, where frost wedging pushes rocks apart when ice expands in cracks and oxidation slowly removes electrons from rocks exposed to oxygen over time.
2) It mentions debris flows seen on a mountainside after exiting a road, leaving scars from the rapid movement of rock and soil.
3) It characterizes environments like a continental creek in California subject to flash flooding, a marine environment at Morrow Bay containing shallow and deep ocean areas, and the transitional beach environment between land and sea.
Field/Lab Assignment Part 2
1) The document contains pictures from various locations that demonstrate different geological concepts such as the San Andreas Fault, chemical and mechanical weathering, erosion, mass wasting, continental, marine, and transitional sedimentary environments, and practical applications of geology such as bridge construction.
2) Specific locations mentioned include Parkfield, CA near the San Andreas Fault, Pismo State Beach demonstrating mechanical weathering and transitional environments, the town of Three Rocks, CA as an example of mass erosion, the San Joaquin River, and bridges over the California Aqueduct.
3) Examples of chemical weathering shown are rusting of metal and oxidation reactions. Mechanical weathering examples are broken down rocks at Pismo State
Filed assignment
This document summarizes a geology field assignment completed by Norma Alvarez. It includes identification and descriptions of 5 rock samples collected from various locations. Samples include phyllite, andesite, granite, and sandstone. Descriptions of field observations of a fault, various weathering processes, mass wasting and erosion events, and different sedimentary environments are also provided. Examples given include frost wedging, oxidation, rock slides, and transitional, continental, and marine environments. The document concludes with photos of canal banks used for irrigation in farming, highlighting the practical use of geology.
Field lab part 2
This bridge outside of Parkfield, California shows evidence of movement along the San Andreas Fault. The guardrail curves and the deck is angled, demonstrating how the fault has caused the bridge to bend. The San Andreas Fault is a strike-slip fault where the Pacific and North American tectonic plates are moving horizontally past one another, with the Pacific plate moving north and the North American plate moving south.
Geology 2 lab Assignment
1) This document contains pictures and descriptions from a geology student's field assignment around Lake Kaweah in California.
2) Pictures show examples of mechanical weathering like frost weathering and root weathering on rocks.
3) Other pictures depict sedimentary environments like streams, beaches, and marine environments, and geological structures like bridges.
4) The student provides context for each picture and learns about geology through the field assignment.
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Field assignment part 2
- 1. Field Assignment Part II By Edward Potter
- 2. Weathering This is an example of chemical weathering on a headstone at False Cape State Park, Virginia Beach, VA This is also an example of chemical weathering of a manhole cover in Virginia Beach, VA
- 3. Mass Wasting/Erosion The picture on the left is is a house, at Sandbridge beach, in Virginia Beach. The ground caved in and sunk everything around it. The picture below is from Millerton Lake.
- 4. Sedimentary Environments Continental. This picture was taken at Stumpy Lake in Virginia Beach, VA
- 5. Sedimentary Environments Marine: This picture was taken at the Oceanfront in Virginia Beach Virginia.
- 6. Sedimentary Environments Transitional: This picture was taken at the Oceanfront in Virginia Beach Virginia; it shows the transition between Continental and Marine.
- 7. Practical Uses of Geology This picture is of a stormwater runoff pond behind my house. Stormwaterponds are becoming a fixture to many residential communities, especially those under new development. Designed to capture all the run-off from parking lots and surrounding areas.
- 8. Practical Uses of Geology The picture on the top is of the entrance to the Chesapeake Bay Bridge Tunnel. The Picture on the Bottom is of the bridge tunnel itself. The water is deep here in Virginia, as well as ships moving in and out of here on a constant basis, so they design “Bridge-Tunnels” they start off as bridges, go into tunnels under the water, and then turn back into bridges on the other side.
- 9. This was a very interesting project, more difficult that I had anticipated, but fun, nonetheless. I did not get to add an example of a fault, as I was unable to witness and document one from Virginia Beach Virginia. I searched the internet and it doesn’t look like there is any here on the East Coast. Not that I found anyway.