Lyme Regis Environmental Improvements
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Transcript Lyme Regis Environmental Improvements
Lyme Regis
No longer Slip-sliding
Away
September 1, 2006
Introduction
Location
England
Southwest Coast
Dorset
Jurassic Coast World
Heritage Site
Exposed to severe
winter storms
West, 2006
Stormy Weather
Undated, 1970’s storm
Source: West, 2006
Calm Weather
The Geology of Lyme Regis
Greensand
Clay
Shale
Blue Lias
Steep slope
The Beginnings of a Landslip
Charmouth Road Car
Park
Asphalt is contributing
to landslip
Work underway to
improve drainage
system
The Black Venn
Between Lyme Regis
and Charmouth
Mostly Clay and
Shales with Beef
Prone to landslides
Rich source of fossils
The Blue Lias
West of Lyme Regis at
Monmouth Bay
Greensand
Clay
Limestone
Landslides
1962 Langmoor
Gardens
Caused by
construction activities
The area was regraded and Langmoor
gardens were
established
The Spittles
East of Lyme Regis
The whole system was
reactivated in 1986
Long-shore drift interrupted
Beach buildup
Monmouth beach
Increased protection
Beach depletion
Shingle supply
interrupted
This results in depletion
The depleted beach(1960’s) and
breached seawall (1974)
Coastal Defenses - The Cobb
Coastal Reinforcements
Beacon Rocks extended by 110 meters
North wall rockery realigned
Added rock armor at Cobb Gate
New jetties at Lister Gardens and Cobb
Gate
Beach replenishments
Sand and shingle
Raised beach level by 2 meters
Beacon Rocks
Armor rocks:
11,000 tonnes core rock, 2 - 5 tonnes each
26,500 tonnes armor, 9 - 18 tonnes each
Source: Norwegian granite
Byproduct
of granite counter top industry
Shingle (pebbles):
72,000 tonnes
Source: Isle of Wight
Sand:
37,000 tonnes
Source: northern France
Precast concrete:
Source: UK
Limestone facing
Source: China
Rock Armor at Cobb Gate Jetty
Finishing up at Cobb Gate Jetty
Reinforcements at Cobb Gate
Lyme Harbor beach restored
Work continues at Langmoor
Gardens
Slope stabilization
Began in 2005, scheduled completion 2007
Major engineering effort involved
considerations for seismic stability
Only small equipment allowed until slope
was sufficiently stabilized
Gradual increase in machinery size based
on monitoring
1,150 auger-cast piling
Drilled holes thru clay into bedrock
Filled with concrete and reinforcement
Act as dowels to hold slope
Soil nails
Similar to piling but horizontal
2,300 meters drainage
Counterforts - at base
Drilled drains -in hill
French drains - below car park
Conclusion
Phase II construction is nearly complete
Coastal defenses
Slope stabilization
Increased security for town
Increased income due to tourism
Cost to maintain will be less than the cost of
emergency repairs