Boscastle PEE guide
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The document discusses the causes and effects of flooding in the village of Boscastle in Cornwall, England. Some of the key causes included heavy rainfall of 180mm in three hours, saturated ground from previous stormy weather, and the village's location within the Valency valley which acted as a funnel for flood waters. The flash flooding gave little time for people to prepare or evacuate, and flood waters inundated the main car park located next to the river. Examples of effects included huge volumes of water flowing through the town and increased surface runoff from impermeable surfaces like roads.
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1GEO347 – Climatic Geomorphology Exercise #1 – Hills.docx
1
GEO347 – Climatic Geomorphology
Exercise #1 – Hillslope Stability: Analyses and Applications
Handed out: February 19, 2020
Write-up due: March 6, 2020
Purpose:
This exercise explores more deeply some of the mass wasting concepts covered in lectures. In Part (A)
we will make observations and collect some data for use in Part (B).
General Geologic Setting. Montara Mountain and the Devil's Slide area are located within the
California Coast Range Geomorphic Province, which consists of a series of northwesterly trending
ridges and valleys formed by compressional tectonic forces. The geologic units located within the study
area consist of Cretaceous Montara Mountain granodiorite overlain with Paleocene age sedimentary
rock. Granodiorite is a coarse-grained plutonic rock consisting of quartz, plagioclase and potassium
feldspar, biotite, hornblende, or, more rarely pyroxene. It is in fault contact with the overlying
sedimentary rock consisting of sandstone, shale, and conglomerate. The sedimentary rock within the
study area is steeply dipping, folded, faulted, and further disturbed by repeated episodes of landslides.
The fault separating these two units is an inactive, oblique fault that descends northwest across the cliff
face. Colluvium and shallow slide debris are found throughout the slide, above and below the roadway.
Source: U.S. Department of Transpiration and The State of California, Department of Transportation,
1986.
Part A (40 points) – To be worked on in class and written up outside class:
1. For this question we will examine a long-standing problem stretch of highway #1 along the California
coastline north of Half Moon Bay. The general geologic setting is described below, and a photograph is
provided separately (also posted on UBlearns). After reading about the general geologic setting, look
carefully at the left side of the photo.
Find the bedding (layering) of the sedimentary rocks. Don’t be confused by the ravines eroded by water.
Which way does the bedding dip? Explain why this makes the area more vulnerable to landslides. (Hint:
See Table 1, reproduced from Ritter et al. 2011)
2. For this question we will measure slopes at Devil’s Slide. The method for calculating slope from
topographic maps is shown in Figure 1. Figure 2 shows a portion of the Montara Mountain USGS 7.5-
minute Quadrangle. A scale is provided as this image does not retain the original 1:24K scale. Points (A)
and (B) show locations where landslides have occurred several times of the past 30 years.
Determine the average slope of the land surface from the shore to the highway at (A) and (B). Repeat for
an equal horizontal distance above the highway. Be sure to get your group’s numbers written down for
later calculations. Compare the slopes at (A) and (B) to those on the headland (C). Discuss why the
headland denudation rates are lower than those at (A) and (B).
2
tan 𝛼 = !!
.
1GEO347 – Climatic Geomorphology Exercise #1 – Hills.docx
1
GEO347 – Climatic Geomorphology
Exercise #1 – Hillslope Stability: Analyses and Applications
Handed out: February 19, 2020
Write-up due: March 6, 2020
Purpose:
This exercise explores more deeply some of the mass wasting concepts covered in lectures. In Part (A)
we will make observations and collect some data for use in Part (B).
General Geologic Setting. Montara Mountain and the Devil's Slide area are located within the
California Coast Range Geomorphic Province, which consists of a series of northwesterly trending
ridges and valleys formed by compressional tectonic forces. The geologic units located within the study
area consist of Cretaceous Montara Mountain granodiorite overlain with Paleocene age sedimentary
rock. Granodiorite is a coarse-grained plutonic rock consisting of quartz, plagioclase and potassium
feldspar, biotite, hornblende, or, more rarely pyroxene. It is in fault contact with the overlying
sedimentary rock consisting of sandstone, shale, and conglomerate. The sedimentary rock within the
study area is steeply dipping, folded, faulted, and further disturbed by repeated episodes of landslides.
The fault separating these two units is an inactive, oblique fault that descends northwest across the cliff
face. Colluvium and shallow slide debris are found throughout the slide, above and below the roadway.
Source: U.S. Department of Transpiration and The State of California, Department of Transportation,
1986.
Part A (40 points) – To be worked on in class and written up outside class:
1. For this question we will examine a long-standing problem stretch of highway #1 along the California
coastline north of Half Moon Bay. The general geologic setting is described below, and a photograph is
provided separately (also posted on UBlearns). After reading about the general geologic setting, look
carefully at the left side of the photo.
Find the bedding (layering) of the sedimentary rocks. Don’t be confused by the ravines eroded by water.
Which way does the bedding dip? Explain why this makes the area more vulnerable to landslides. (Hint:
See Table 1, reproduced from Ritter et al. 2011)
2. For this question we will measure slopes at Devil’s Slide. The method for calculating slope from
topographic maps is shown in Figure 1. Figure 2 shows a portion of the Montara Mountain USGS 7.5-
minute Quadrangle. A scale is provided as this image does not retain the original 1:24K scale. Points (A)
and (B) show locations where landslides have occurred several times of the past 30 years.
Determine the average slope of the land surface from the shore to the highway at (A) and (B). Repeat for
an equal horizontal distance above the highway. Be sure to get your group’s numbers written down for
later calculations. Compare the slopes at (A) and (B) to those on the headland (C). Discuss why the
headland denudation rates are lower than those at (A) and (B).
2
tan 𝛼 = !!
!!
..
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1GEO347 – Climatic Geomorphology Exercise #1 – Hills.docx
1
GEO347 – Climatic Geomorphology
Exercise #1 – Hillslope Stability: Analyses and Applications
Handed out: February 19, 2020
Write-up due: March 6, 2020
Purpose:
This exercise explores more deeply some of the mass wasting concepts covered in lectures. In Part (A)
we will make observations and collect some data for use in Part (B).
General Geologic Setting. Montara Mountain and the Devil's Slide area are located within the
California Coast Range Geomorphic Province, which consists of a series of northwesterly trending
ridges and valleys formed by compressional tectonic forces. The geologic units located within the study
area consist of Cretaceous Montara Mountain granodiorite overlain with Paleocene age sedimentary
rock. Granodiorite is a coarse-grained plutonic rock consisting of quartz, plagioclase and potassium
feldspar, biotite, hornblende, or, more rarely pyroxene. It is in fault contact with the overlying
sedimentary rock consisting of sandstone, shale, and conglomerate. The sedimentary rock within the
study area is steeply dipping, folded, faulted, and further disturbed by repeated episodes of landslides.
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face. Colluvium and shallow slide debris are found throughout the slide, above and below the roadway.
Source: U.S. Department of Transpiration and The State of California, Department of Transportation,
1986.
Part A (40 points) – To be worked on in class and written up outside class:
1. For this question we will examine a long-standing problem stretch of highway #1 along the California
coastline north of Half Moon Bay. The general geologic setting is described below, and a photograph is
provided separately (also posted on UBlearns). After reading about the general geologic setting, look
carefully at the left side of the photo.
Find the bedding (layering) of the sedimentary rocks. Don’t be confused by the ravines eroded by water.
Which way does the bedding dip? Explain why this makes the area more vulnerable to landslides. (Hint:
See Table 1, reproduced from Ritter et al. 2011)
2. For this question we will measure slopes at Devil’s Slide. The method for calculating slope from
topographic maps is shown in Figure 1. Figure 2 shows a portion of the Montara Mountain USGS 7.5-
minute Quadrangle. A scale is provided as this image does not retain the original 1:24K scale. Points (A)
and (B) show locations where landslides have occurred several times of the past 30 years.
Determine the average slope of the land surface from the shore to the highway at (A) and (B). Repeat for
an equal horizontal distance above the highway. Be sure to get your group’s numbers written down for
later calculations. Compare the slopes at (A) and (B) to those on the headland (C). Discuss why the
headland denudation rates are lower than those at (A) and (B).
2
tan 𝛼 = !!
.
1GEO347 – Climatic Geomorphology Exercise #1 – Hills.docx
1
GEO347 – Climatic Geomorphology
Exercise #1 – Hillslope Stability: Analyses and Applications
Handed out: February 19, 2020
Write-up due: March 6, 2020
Purpose:
This exercise explores more deeply some of the mass wasting concepts covered in lectures. In Part (A)
we will make observations and collect some data for use in Part (B).
General Geologic Setting. Montara Mountain and the Devil's Slide area are located within the
California Coast Range Geomorphic Province, which consists of a series of northwesterly trending
ridges and valleys formed by compressional tectonic forces. The geologic units located within the study
area consist of Cretaceous Montara Mountain granodiorite overlain with Paleocene age sedimentary
rock. Granodiorite is a coarse-grained plutonic rock consisting of quartz, plagioclase and potassium
feldspar, biotite, hornblende, or, more rarely pyroxene. It is in fault contact with the overlying
sedimentary rock consisting of sandstone, shale, and conglomerate. The sedimentary rock within the
study area is steeply dipping, folded, faulted, and further disturbed by repeated episodes of landslides.
The fault separating these two units is an inactive, oblique fault that descends northwest across the cliff
face. Colluvium and shallow slide debris are found throughout the slide, above and below the roadway.
Source: U.S. Department of Transpiration and The State of California, Department of Transportation,
1986.
Part A (40 points) – To be worked on in class and written up outside class:
1. For this question we will examine a long-standing problem stretch of highway #1 along the California
coastline north of Half Moon Bay. The general geologic setting is described below, and a photograph is
provided separately (also posted on UBlearns). After reading about the general geologic setting, look
carefully at the left side of the photo.
Find the bedding (layering) of the sedimentary rocks. Don’t be confused by the ravines eroded by water.
Which way does the bedding dip? Explain why this makes the area more vulnerable to landslides. (Hint:
See Table 1, reproduced from Ritter et al. 2011)
2. For this question we will measure slopes at Devil’s Slide. The method for calculating slope from
topographic maps is shown in Figure 1. Figure 2 shows a portion of the Montara Mountain USGS 7.5-
minute Quadrangle. A scale is provided as this image does not retain the original 1:24K scale. Points (A)
and (B) show locations where landslides have occurred several times of the past 30 years.
Determine the average slope of the land surface from the shore to the highway at (A) and (B). Repeat for
an equal horizontal distance above the highway. Be sure to get your group’s numbers written down for
later calculations. Compare the slopes at (A) and (B) to those on the headland (C). Discuss why the
headland denudation rates are lower than those at (A) and (B).
2
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Amphibious Flood Protecting House for River Side Area
The – It is well known that “FLOODS ARE ACTS OF GOD, BUT FLOOD LOSSES ARE LARGELY ACTS OF MAN.” We are all living in the 21st century and are on the edge of rapidly increasing population. The population on Earth has increased from 1 billion to 7 billion in the previous 3 centuries and is still on the verge of increasing with no signs of reducing by any means. The increasing number of population leads to their shelter and there shelter causes and affects the environment in indefinite number of ways. A house can cost someone in some bucks, but it costs the environment of Mother Nature more than any other resources. Having knowledge of all these the human being has got no plans to stop, But in the end it all comes back in some or the other ways. Nature always treats you in response, the same way you do. Harms to nature costs Flood, Earthquakes, Hurricanes, tsunamis and other geological natural disasters. The First thing that gets destroyed in these disasters are Habitats. Yes, be it Human or other species the habitat of a human being lies around homes, and these are the first target by the disasters. The Indian Continental alone has spent a total of 3.9 B dollars in the 65 yrs. of its independence, only when the skies cursed. It is a basic need to encounter the problem of losses due to floods, and as said in the phrase the flood losses are largely and solely the act of man itself. Prof. Sachin L. Desale | Prof. Sachin B. Kajabe | Sachin L. Kankute | Sandip M. Narote | Tushar S. Thakare "Amphibious Flood Protecting House for River Side Area" Published in International Journal of Trend in Scientific Research and Development (ijtsrd), ISSN: 2456-6470, Volume-6 | Issue-4 , June 2022, URL: https://www.ijtsrd.com/papers/ijtsrd50145.pdf Paper URL: https://www.ijtsrd.com/engineering/civil-engineering/50145/amphibious-flood-protecting-house-for-river-side-area/prof-sachin-l-desale
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Boscastle PEE guide
- 1. Developing extended writing skills – the Boscastle floods © www.teachitgeography.co.uk 2016 25506 Page 1 of 2 Student tasks 1. Underline any geographical keywords. Do you understand what they mean? 2. Can you circle below all the causes of flooding? (These are your POINTS) Extension: Can you differentiate between the human and physical causes? 3. Shade the boxes that show all the EXAMPLES. 4. Draw a line to link the EXAMPLES to the correct POINT. 5. In another colour, link the correct EXPLANATION to the correct POINT and EXAMPLE. This shape means that the land acted as a funnel, directing vast volumes of water into the village The village of Boscastle is located within the Valency valley Heavy precipitation This flash flood meant that people had very little time to prepare or evacuate This meant that when the volume of water in the rivers increased, it lead to huge volumes of water flowing through the town Urbanisation This meant that surface runoff increased, as excess water could no longer soak into the soil Boscastle is at the confluence (where tributaries meet) of three rivers: the Valency, Jordan, and Paradise 180 mm of rainfall fell in three hours The entire south west of England had been battered with stormy weather over the days leading up to the flood The main car park in Boscastle is located right next to the river Large drainage basin This meant that impermeable surfaces like tarmac, increased the spread of floodwater into the village Steep valley sides Saturated ground 6. Complete a paragraph to explain one of the causes of flooding. POINT: One of the causes of flooding in Boscastle was… EXAMPLE: An example of this is… EXPLAIN: This means that… 7. Complete another PEE paragraph using a different cause. Boscastle before the floods © Matthew Hunt, 2003, flic.kr/p/Lh7B
- 2. Developing extended writing skills – the Boscastle floods © www.teachitgeography.co.uk 2016 25506 Page 2 of 2 Extension task Use this PPE technique in your essay for the EFFECTS and RESPONSES of your chosen case study. Think about using quotes from people directly involved in the flooding. Assessment exercise Imagine you are a reporter for a newspaper. Your task is to report on flooding in the UK using the PPE framework. You can focus on a particular place or wider region. Use the following questions to structure your report: 1. Where is the flood? You should include location maps. 2. What are the causes of the floods? You should include keywords covered in class. 3. What are the effects of the floods? You should include annotated photographs / specific case study detail / quotes from local people. 4. How have people responded to the flood? You should include local people, rescue services and the Environment Agency. Useful Websites Recent floods – www.theguardian.com/environment/flooding The 2015–16 Great Britain and Ireland floods – en.wikipedia.org/wiki/2015%E2%80%9316_Great_Britain_and_Ireland_floods The Environment Agency flood information service – flood-warning-information.service.gov.uk/ The Cumbria floods of December 2015 – www.bbc.co.uk/news/uk-england-cumbria-35159816 Flooding in Lancashire and Yorkshire in December 2015 – www.telegraph.co.uk/news/weather/12069820/Severe-floods-hit-Lancashire-and-West-Yorkshire- in-pictures.html?frame=3537632 Useful keywords and phrases: impermeable surface runoff saturated Environment Agency flood defence high tide precipitation flood warning evacuation fire and rescue compensation insurance Government Flooding in York © Michael Wilson, 2007 commons.wikimedia.org/wiki/File:June_floods_Yorkshi re_canoes.jpg