Geomorphological evolution of Montserrat (West Indies):
1 / 39

Geomorphological evolution of Montserrat (West Indies): importance of flank collapse and erosional processes - PowerPoint PPT Presentation

  • Uploaded on

Geomorphological evolution of Montserrat (West Indies): importance of flank collapse and erosional processes. Authors: A. Le Friant, C.L. Harford. C. Deplus, G. Boudon, R.S.J. Sparks, R.A. Herd & J.C. Komorowski. What is it essentially?.

I am the owner, or an agent authorized to act on behalf of the owner, of the copyrighted work described.
Download Presentation

PowerPoint Slideshow about 'Geomorphological evolution of Montserrat (West Indies): importance of flank collapse and erosional processes' - Gideon

An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.

- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -
Presentation Transcript
Slide1 l.jpg

Geomorphological evolution of Montserrat (West Indies): importance of flank collapse and erosional processes

Authors: A. Le Friant, C.L. Harford. C. Deplus, G. Boudon, R.S.J. Sparks, R.A. Herd & J.C. Komorowski

What is it essentially l.jpg
What is it essentially?

  • The paper looks at the Montserrat island in the West Indies and then through certain studies of the morphology of the island and surrounding sea floor the authors proposed three stages of evolution for andesitic volcanoes in a marine setting.

Points covered l.jpg
Points covered

  • Geological setting – where is Montserrat?

  • Morphology and important observation

    • Island.

  • Depositional environment

  • Discussion and conclusion of the paper

Geological setting l.jpg

Located 16º 45’N and 62º 10’ W

Forms part of the Lesser Antilles fore arc.

The N.American Plate subducted under the Caribbean Plate

Geological Setting

Slide5 l.jpg

Tectonic setting of Montserrat

Slide6 l.jpg

Montserrat Position – location of volcanoes in the Lesser Antilles arc

Slide7 l.jpg

Montserrat. Taken from google earth Antilles arc


The summit of Soufrière Hills volcano towers above the streets of Plymouth,

Photo by Cynthia Gardner, 1995 (U.S. Geological Survey).

Slide8 l.jpg

Topographic model of Montserrat:Courtesy of Dr. Ian C.F.Stewart

Events occurring l.jpg
Events occurring: Antilles arc

  • Active Volcano – South Soufrière Hills. Andesitic stratovolvano that is dome forming.

  • Silver Hills is an extinct Basalt-Andesitic volcano(Harford,2002)

  • Deposits are characterized by lava domes, lava talus breccias and tephra falls. Flank and dome collapse events form pyroclastic flows.

Slide11 l.jpg

Morphology Antilles arc

  • Look at morphology of each main massif separately

    • Silver Hills

    • Centre Hills

    • Soufière Hills and South Soufière Hills

Topographic model of Montserrat:Courtesy of Dr. Ian C.F.Stewart

Island morphology l.jpg
Island Morphology Antilles arc

  • Sliver Hills (2600-1200ka)

    • Characterized by high amounts of erosion (deeply eroded)

    • Highest peak of 403m

  • Centre Hills (950-550ka)

    • Characterized by high cliffs – mainly coastal cliffs

    • Highest peak of 741m (Kathy Hill)

    • 2 Discontinuities that are caused by flank collapse (Sa & Sb on fig 2b)

    • Discontinuities defined by the hydrographic system

Island morphology14 l.jpg
Island Morphology Antilles arc

  • Soufrière Hills and South Soufrière Hills

    • Active volcano

    • Less erosion but more faults - unstable

    • Main features on the south side of island:

      • English’s Crater (1km x 1.6km) due to flank failure

      • The Scar Features (Sb. fig2b)

        • Forms discontinuities that divides Soufrière Hills and South Soufrière Hills. All have steep scarps.

      • 3 large imbricated horse shoe depression structures all caused by flank failure (Sc on fig 2 and fig 3)

      • Large Debris avalanches (Boudon 2002)

Slide15 l.jpg

Castle Peak dome and English's crater 1995. Antilles arc

Simplified map showing the northern extent of the pyroclastic flow and surge deposits from the June 25, 1997, dome-collapse and explosion event at Soufriere Hills volcano, Montserrat (modified from from MVO Special Report 03 on June 29, 1997; see anchor below).

Scar features l.jpg
Scar Features Antilles arc

A. Le Friant (Paper Research pg 150)

Slide17 l.jpg

Crater in top of growing dome Oct 1997. Antilles arc

Delta formed by pyrolaccstic flow.

Google Earth

  • Recent Eruption of the active volcano

    • Formed a lava dome at height of 1100m

    • Valleys are filled by pyroclastic flows as well as block and ash flows. These flows are also responsible for the deltas and fans formed.

Ocean floor morphology l.jpg
Ocean Floor Morphology Antilles arc

  • Shallow Shelf of 20- 60m depth (Fig 4a,b)

  • Canyons and gullies 100m deep (West)

  • Gentle slope <4º (East of the island)

    • Hummocky structures stretch S-N (750m – 1000m deep)

  • Slope of seafloor along island

    • Concave up slope

      • More liner towards the active sites of the island

      • More concave towards extinct volcanoes (Northwards)

Slide21 l.jpg

Main Instabilities Antilles arc

  • Debris Avalanche Deposits

    • Characterized by rough hummocky topography

    • The avalanche deposits are triggered by flank failure and dome collapse events

Slide22 l.jpg

  • Flank Collapse Events Antilles arc

    • 4 types occur on Montserrat

      • English Crater Event

        • Due to flow erosion of sediments and forms the Tar River Fan

      • South Soufrière Hills - Soufrière Hills events

        • Due to submarine and subaerial flank failures

        • The events caused the flank scar see as Sc on fig2

      • Other Events

        • submarine failure

        • the collapse of the infill of the horseshoe features

      • Submarine embayment

        • Submarine failure of accumulated sediments on the shelf

Slide23 l.jpg

Zoom in of fig 2. Showing the South Soufriere Hills –Soufriere Hills Scar features.

Slide24 l.jpg

  • Pyroclastic flows –Soufriere Hills Scar features. classified as 2 types

    • Pyroclastic flow deposited on land

      • Fills Valleys

    • Pyroclastic flow deposited in sea

    • 80% product eventually ends up in the sea.

      • Forms the deltas that can be as big as 1km² in area

      • Tar River and White River

    • Products of volcanic activity, dome collapse (e.g 12 July 2003) and also flank failure

Slide25 l.jpg

Reference : Pyroclastic Flow: –Soufriere Hills Scar features.

Pyroclastic flow l.jpg
Pyroclastic Flow –Soufriere Hills Scar features.

Video Clip of pyroclastic flow into the ocean:

Slide27 l.jpg

Pyroclastic flows from Montserrat dome collapses have flowed down the White River creating a new delta where they entered the sea. It is uncertain if this delta will survive or be eroded by seawaves. Photograph copyrighted and provided by Steve O'Meara of Volcano Watch International.

Discussion l.jpg

Long Term Surface Erosion Rate (ER) down the

Using information form Silver Hills

The volume loss of 15km³ over 1200ka

= 0.0125km³/ka


East coast sea cliffs, showing a number of sequences of pyroclastic flows.

Discussion29 l.jpg

Magma Production Rate down the

South Soufrière Hills - Soufrière Hills

Oldest preserved base of volcano 174ka

Thought that 50% eruption products end up in the ocean (before 12 July 03)

Vt = Vp + Vm+Ve + Vc

Minimum time averaged production rate = 0.17km³/ka

(400times lower then the current estimated rate at 70km³/ka)

Means that production was a small part in history (Wage & Isaacs 1988)

Vt = total produced magma

Vp = actual preserved subearial volume of the volcano = 12km³

Vm = erupted volume into sea (50% of Vt) = 15km³

Ve = material that has been eroded at ER/174ka = 2.2km³

Vc = collapsed volume = 1km³

Therefore Vt ~ 30km³ over 174ka


Slide30 l.jpg

  • ER vs. Production rate (PR) down the

    • ER (0.0125km³/ka) = 7% PR (0.17km³/ka)

      • Most obviously the PR>ER

      • Shows that most erupted material is deposited straight into the ocean

      • South Soufrière Hills - Soufrière Hills attributes 6% of the Lesser Antilles arc magma production

  • Sea Deposits Rate

    • The calculated rate of 0.085km³/ka can be modified to 0.11km³/ka due to episodic events such as

      • Debris avalanches, flank failure and pyroclastic flows also affecting land drainage

      • This rate shows that over the last 174ka, 19km³ (65%Vt) of volcanic products are deposited on the sea floor

      • Volcanic sediments contributed 80% of volcanic products of the island arc (Sigurdsson 1980)

Morphological evolution of the island l.jpg
Morphological evolution of the island down the

  • Interpreted in 3 stages

    • Stage 1

      • Submarine growth

      • ER has little effect

      • The PR >> ER

      • Kick ‘em Jenny (southern part of the arc) at this stage (Sigurdsson & Sparks 1979)

Slide32 l.jpg

Kick andJenny down the

Image by Doug Martin, 1996 (NOAA, courtesy of Seismic Research Unit, University of West Indies).

Slide33 l.jpg

  • Stage 2 down the

    • Active subaerial growth

    • PR > ER

    • Magma extrusion takes place – subaerial edifice built

    • South Soufrière Hills - Soufrière Hills is an example

    • High sediment supply to oceans

      • Flank collapse and pyroclastic flows

    • The large flank collapse events shape the island

      • English’s crater event (4ka)

    • The hydrological alteration is the main cause of flank collapse

    • Only stage that pyroclastic flows occur

Slide34 l.jpg

  • Stage 3 down the

    • Extinction and erosion

    • When active volcano becomes extinct

    • Here PR < ER

    • Land material is weathered into the ocean which forms a shallow shelf environment

    • Submarine failure and collapse events must be triggered by tectonic events as there is no volcanic activity for sedimentary loading

    • Silver and Centre Hills of Montserrat are good examples. (Noting the shelf north of the island)

Slide35 l.jpg

Fig 10a. Evolution of Montserrat down the

A. Le Friant (Paper Research pg 159)

Slide36 l.jpg

Fig 10b. Evolution of Montserrat down the

A. Le Friant (Paper Research pg 159)

Slide37 l.jpg

Video Clip of pyroclastic flows into the ocean of Montserrat – Tar River

Slide38 l.jpg

South Soufriere Hills - Soufriere Hills volcanic eruption at night


Bibliography l.jpg
Bibliography night

  • Wikipedia – free online encyclopedia

  • GoogleEarth