I've only come across territorial acknowledge via Twitter recently. I feel guilty that it was only recently and not at the start of the academic journey. Although that guilt can easily be replaced with: why haven't I seen it talked about in this country? I mean…I have a few opinions as to why, but I will leave the politics of colonialism/post-colonialism to others.
I found a few sites on how terrirotial acknowledgement is approached by them (links at the end) and found that they were based on respect and building positive bridges based on the land they are living on. Although the UK won't be able to exactly do this, what if our research is in a country/region that did belong to indigneous groups before European contact? I would see it as a strength that we are trying to build bridges that we face up to our country's past, acknowledge that there were negative consequences and that we need to develop new healthier relationships.
Here is my acknowledgement example:
"This thesis has been conducted on the Caribbean Island of St. Vincent and the Grenadines, that once belonged to the Kalinago, who call the island Youloumain, and the Garifuna, who call the island Yurumei. They originally inhabited the coastal areas of the island however, due to British colonialisation they were forced inland and north near the volcano La Soufrière, in which unfortunately the original name given by the Kalinago and Garifuna has been lost. This has ever since placed the descendants of the two groups at higher risk of La Soufrière’s explosive eruptions. At the end of the Second Carib War in 1797, many Garifuna were exiled to Roatán, an island of Honduras. Exiled descendants now live in Belize, and continue to fight to return to their homeland. It is without a doubt, that the influence of colonialisation and creolisation has caused the indigenous knowledge of the island and the hazards that it is exposed to, to be omitted from written historical records, which do not reflect the enduring sovereignty of the Kalinago and Garifuna people. The island still belongs to them, but is no longer predominately occupied by them. The author has endeavoured to represent the groups’ voice in the narrative of this thesis."
Kalinago – displaced the Arawak in the Lesser Antilles, migrating from Venezuela (called "Yellow/Red Caribs"
Garifuna – runaway African slaves (supposedly Spanish) who intermarried with the Kalinago (called "Black Caribs")
I think it will go before or after my main acknowledgements. I suppose I am making the effort to do this is because I know my family and ancestors are from previously colonised countries (St. Vincent, Jamaica, Cuba, Cameroon and possibly India) and one thing my grandfather always tells me is: "We are Carib, our blood is Carib" but unfortunately, I do not know if I am Kalinago or Garifuna.
The acknowledgement humanises and lets people know you understand the past, present and future of the communities that were in certain areas before others came along. We should not feel ashamed in doing it and we certainly should not keep pushing some groups of people out. We should acknowledge the territories in which we live and/or work upon.
I apologise for the lack of posts…been busy writing away!
I have completed drafts on chapters 4 and 5, and currently working away on chapter 6. Chapter 4 I reconstructed the 1812, 1902 and 1979 eruptions of La Soufrière using archive sources and interviews. Chapter 5 was the impacts of the eruptions on the agricultural industry. Chapter 6 I am focusing on the evolving social risk and geoculture across the 168 years.
Chapter 6 is a bit of a challenge, but I have a lot of fascinating stuff to share once it all comes together!
In other news:
I have applied for a Visting Researcher position but I won’t say anything more!
I will be attending the IRDR 7th Annual Conference in July
I’ll also be attending a ‘Building Resilience to Geohazards in the Face of Uncertainty’ hosted by the Geological Society in September
That’s all for now! I’ll be using my new mantra to get through the next few months:
Because of the whole faff of the Oscars (honestly, why it was headline news I’ll never know), some may have missed something awesome: Mt Etna in Sicily started producing Strombolian activity at a new scoria cone at the Southeast crater last night.
Here is a link to a very stable live video feed of the ongoing eruption, the featured photo is a screenshot of tonight’s activity. Enjoy!
Hello! The Inthecompanyofvolcanoes blogging ladies have called upon women who do volcanology around the world (including myself) to share why love what they do and encouraging words to girls (and boys) to get into STEM and geoscience.
It’s an inspiring read with so many fantastic women featured, so do check it out and share with kids! You can find it here.
It will be updated as time goes on, so do check it out every now and then!
In the ideal world as researchers, we all want our findings to reach the public and be understood. How clear (or unclear) we present our research outside of the science domain could be a reason why it gets interpreted in a way we did not intend.
Near the end of last year, the Campi Flegrei Caldera in Italy, made the news- for better or for worse. The positive part (from a scientific perspective) was that the news came about because a journal article was published and picked up by the media. The less positive part was that in some cases (not all), the interpretation of this news was all doom and gloom. I will look at 1 tabloid and 1 broadsheet based newspapers that reported the news to showcase this.
Critical degassing pressure
The study in question was by Chiodini et al. (2016). They used a volatile (gas) saturation model based on Papale et al. (2006) to illustrate the decompression of magma can reach the ‘critical degassing pressure’, affecting the magma’s ability to release water and convect heat. The sub-disciplines of geochemistry and geophyics were used to understand this. In order to make the experiment applicable to the ‘real world’, Campi Flegrei was used as the main example but, there were also references to Rabaul in Papua New Guinea (Acocella et al., 2015) and Sierra Negra in the Galapagos (Segall, 2013). When I can find them, I will update this post to blogs that go into more detail about this paper.
As a social volcanologist, I am more interested in how people interpreted, responded and communicated the following headlines:
Daily Mail Online: Is the SUPERVOLCANO under Naples about to blow? Campi Flegrei crater shows signs of ‘reawakening’
Shares: 326 (17/01/16)
Comments: 82 (17/01/16)
The article was actually quite brief, and gave a basic version of the main findings. This is understandable and a common practice when communicating information from research to the public. However, the main thing that got my attention was SUPERVOLCANO. The term supervolcano is used to describe a volcano that has produced at least one explosive “supereruption” – that is, an eruption that has a volcanic explosivity index (VEI) 8 or higher, according to Miller and Wark (2008). Other factors that make a volcano “super” are:
The ejection of volcanic material has to be greater than 105kg/450 km3 (Sparks et al., 2005; Self, 2006);
Relatively shortlived (Francis and Oppenheimer, 2004; Mason et al., 2004);
Produce deposits 1000 km3 or more (Miller and Wark, 2008).
Most people are aware of the Yellowstone supervolcano complex, and that is where I think people had jumped to conclusions. Key point that I believe was overlooked was a short quote by Chiodini found in the article:”It is not possible at this time to say when – or if – the volcano will erupt anew” but he then does say if it did. Our science today is not 100% accurate that we can have an exact date and time when an eruption will occur, so communicating the uncertainty is important.
The Guardian: Volcano near Naples showing signs of reawakening
Shares: 4,023 (17/01/16)
Comments: 121 (17/01/16)
A noticeable difference on first glance is the less dramatic headline but, also the significant number of shares and comments.
The summary of findings was essentially the same to the tabloid but, upon reading it the language used does not betray the same level of concern. It presented the facts without using the word “supervolcano”, but interestingly at the end reminds us of the 79AD eruption of Vesuvius. The same quote of Chiodini was used however, it was extended to include the importance of continued research: “Chiodini said there was an urgent need to obtain a better understanding of Campi Flegrei’s behaviour because of the risk to such a dense urban population”. There is plenty of research being done out there on understanding Campi Flegrei, as well as to better inform the public.
Perhaps it is down to more than just knowledge of volcanism (and the particular volcano in question). In the UK, (and perhaps elsewhere, please let me know what it is like in your countries!) it is well known that there are clear divisions in the types of people who read certain newspapers (tabloid versus broadsheet). Maybe it depends on how trustworthy the sources of information are, in the context of hazard communication. With all the issues of fake news of late, this is perhaps important to consider for the future when it comes to communicating about natural disasters and research. For researchers it is important to consider how we communicate our research and in particular uncertainity. Maybe as part of our development as academics, science communication and public engagement should be taught to us by scientists who good at doing so (e.g. Brian Cox, Iain Stewart, David Attenborough, Steven Hawking…where are the famous women STEM communicators?!).
When I heard this news, one of my thoughts was how did the people in Naples and Italy in general respond to this? I have read and heard about the ways volcanologists and key stakeholders involved in managing potential future activity for Campi Flegrei. A noticeable thing I have gathered is that the city of Naples is a very sensitive and challenging situation. There is an expanding population in the vicinity of a famous active volcano that last erupted in 1944 (Vesuvius), but fortunately was not as destructive as the 79AD eruption, as well as Campi Flegrei. Naples is a tourist attraction, I for one have been there on a holiday before heading out to fieldwork on Mt Etna. It is risky, and raises more questions.
To get an idea how the people exposed to this area perceive Campi Flegrei, there was a volcanic risk perception study done by Ricci et al. (2013) – which was a great help for my own volcanic risk perception study on St Vincent. Despite a high confidence in the volcanologists, it was found that there was a low saliency (level of importance) towards the hazards of Campi Flegrei, lack of awareness of the risks, and little information regarding the hazards and risks. There was also a low confidence in the local authorities, which hints that preparedness for a future potential volcanic crisis at Campi Flegrei is low. It was surprising the similarities of their results to mine.
This is not to say that the exposed population is not prepared, but it has and will need continued discussions between volcanologists, local authorties and the community in order to increase the preparedness level. There is time to improve preparedness, it is just a matter of clear communication lines between the different stakeholders.
We can never fully predict how people interpret and react to our research. It perhaps depends on how we communicate our research, by addressing uncertainty and expressing that all efforts are being made to prepare everyone. The paper that stirred up this fuss in itself was interesting science but that was not fully appreciated, mainly due to when changing our research for the public domain, all the important terminology, methods and explanations can be lost, simply because the public do not know the science how we volcanologists know it. Due to the recent topic of fake news, knowing which source is trustworthy may play a greater role in communicating risk in the future. As scientists, our research needs to be clear, and media needs to think more about being sincere in the information that they take from us, not take it just to sell papers.
I would be very interested to hear from people who also saw this news and if you are a volcanologist, did you get any questions? (e.g. can I still go on holiday there).
Acocella V., Di Lorenzo R., Newhall C. and Scandone R. (2015) Caldera unrest: knowledge and perspectives. Rev. Geophys. Vol. 53. Pg. 896-955.
Chiodini G., Paonita A., Aiuppa A., Costa A., Caliro S., De Martino P., Acocella V. and Vandemeulebrouck J. (2016) Magmas near the critical degassing pressure drive volcanic unrest towards a critical state. Nature Communications. Vol. 7. Pg. 1-9 [online] http://www.nature.com/articles/ncomms13712
Francis P. and Oppenheimer C. (2004) Volcanoes. Oxford: Oxford University Press.
Mason B.G., Pyle D.M. and Oppenheimer C. (2004) The size and frequency of the largest explosive eruptions on Earth. Bulletin of Volcanology. Vol. 66. Pg. 735-748.
Miller C.F. and Wark D.A. (2008) Supervolcanoes and their explosive supereruptions. Elements. Vol. 4. Pg. 11-16.
Papael P., Moretti R. and Barbato D. (2006) The compositional dependence of the saturation surface of H2O+CO2 fluids in silicate melts. Chem. Geol. Vol. 229. Pg. 78-95.
Ricci T., Barberi F., Davis M.S., Isaia R. and Nave R. (2013) Volcanic risk perception in the Campi Flegrei area. Journal of volcanology and geothermal research. Vol. 254. Pg. 118-130.
Segall P. (2013) Volcano deformation and eruption forecasting. London: Geological Society, Special Publications.
Self S. (2006) The effects and consequences of very large explosive volcanic eruptions. Phil. Trans. R. Soc. A. Vol. 364. Pg. 2073-2097.
Sparks R.S.J., Self S., Grattan J.P., Oppenheimer C., Pyle D.M. and Rymer H. (2005) Super-eruptions: global effects and future threats. London: Geological Society of London Working Group, The Geological Society.
Upon returning from US fieldwork, I only had a number of weeks to create a conference poster and be on my way to the airport. I was preparing for the Cities on Volcanoes 9 (CoV9) international conference in Puerto Varas, Chile.
I did not know what to expect from the country or the conference. Luckily, both exceeded my expectations. I learned a lot from those who viewed my poster to the talks and other posters, met/made many new contacts and friends, as well as seeing some familiar faces.
CoV is an international conference occurring every 2 years hosted at an alternative city in the vicnity of a volcano(es). The aim is to bring together volcanologists, disaster managers and other researchers concerned with volcanic impacts on society, through the promotion of inter/multi-disciplinary research and establishing colloboration between physical and social scientists, as well as stakeholders like town planners. The particular theme for this year was “Understanding volcanoes and society: the key for risk mitigation”. CoV is part of the IAVCEI (International Association of Volcanology and Chemistry of the Earth’s Interior), which represents all volcanologist throughout the world.
I am not entirely sure how many delegates there was, but it certainly had to be over 500. There was such a rich representation of research across the world, in poster and oral form. There was a lot of them so it was impossible to sit in all talks and speak to everyone about their poster. My priority is to stick the talks and posters that are relevant to my project as well as my research interests, then if I have the time to see/read others, then I will.
Talks/posters I focused on related to agricultural impacts of volcanic eruptions, risk perceptions, historical reconstructions of volcanic eruptions, lahars, PDCs, risk and politics.
The conference itself had opportunities to visit some volcanoes (Chaitén, Calbuco, Osorno and the Laguna del Maule Volcanic Complex) before, during and after the conference. Unfortunately I could not afford any of them but luckily the ones during the conference were included, to visit either Calbuco or Osorno. I chose Calbuco, as it erupted last year. As this was a recent eruption that was on the ‘door step’ of Puerto Varas, it was talked about a lot at the conference. Wired has a nice summary of the activity.
We went to an area that was impacted by lahars, but a year on the rivers/streams have been cleared and artifically transformed, mainly by moving the bigger boulders on the banks. There was a primary school in this area…right under Calbuco to be exact. We walked up the river to a destroyed fish farm. The building was still standing, but was far beyond being operational again with the giant boulders that the lahar carried down. Walking up a little bit more we came to the waterfall in which the lahar came down, it was impressive to see if not slightly unnerving that a vast amount of water filled with volcanic material flowing down the river with such severity. The most interesting part was that we went back to the school and got first hand experiences from a number of individuals from the surrounding villages. The main things that I took away from their experiences were:
As farmers, their main priority was to secure their livelihoods. They accepted the risks and did everything they could to save their livestock;
For many, this eruption was the first they experienced, so a lot of things were learnt as the eruption of occurring;
They were fully aware of their needs, but the government did not and tried to impose what they thought they needed and ignoring what the villages really needed. This frustrated the communities and in the end they had little assistance from the government;
Throughout the event and afterwards, they built and maintained community resilience, social cohesion and social networks, key aspects of withstanding hazardous impacts.
Overall, I am so glad I went. I met some great people, learned a lot and have had valuable feedback from those who came to look at my work on the historical impacts of La Soufrière on the agricultural industry. Most importantly, it gave me confidence and belief in my work and that I could be a valuable member of the social volcanology community.
I am looking forward to the next one in 2018, when it returns to Naples! Hopefully I will be a stage to give a talk.
I was in the USA for 2 weeks September-October on a hunt for more archival sources related to the historic eruptions of La Soufrière. I had never been to America before so I got distracted by all the ‘bigness’ of pretty much everything compared to where I grew up and lived in the UK.
I had two aims:
Obtain copies of the diaries of the American Barrister Hugh Keane from the Virginia Historical Society in Richmond, VA and;
Obtain field notebook copies of the American Geologist Dr Edmund Hovey from the American Museum of Natural History in New York City.
I have to say, I was very impressed with what I found.
My first stop was the Virginia Historical Society in Richmond. I was well aware of the rich history the city and the state itself so I was expecting great things.
Hugh Keane was a barrister in St Vincent in the early 1800s, but his family had been on the island since the late 1700s. His diary entries were in most part short (and small) but he does write on the 30th April about the beginings of the 1812 eruption.
Although this is what I came for I did run into a few issues. One is the handwriting, in which I need to take a paleography course at The National Archives in London for (online thankfully). Another was I actually took most of the pages at a wrong angle (oops) making it harder to transcribe. Another is the language and abbreivations he uses. And a big one is that he doesn’t give a day-to-day running commentary on the eruption. Either Hugh was too busy to watch it (he was a barrister during the slavery era) or he got bored of it. Hopefully his entries will provide helpful insights in what the volcanic processes and hazards were, if not to gain an idea what the responses were.
In any case, I got what I went for so I was happy with that. For Edmund Hovey’s collection I did not know what to expect. All I knew was that he was ordered by the American Museum of Natural History to investigate the eruptions of Pelée and Soufrière.
Dr Edmund Hovey was a geologist and at the time, assistant curator in the palaeontology section of the museum.
Once I got to the room where the collection was held (after getting briefly lost in the museum naturally), the curator assisting my search showed me the list of what they had. It looked exciting. A small cool collection was artifacts that Edmund brought back from Martinique:
I got more excited when I opened up the field notebooks:
Anyone who has done a geoscience based degree or course, knows how important a field notebook is. I was quite impressed with the level of detail Edmund went into, like a true geologist: time, date, location, and detailed descriptions of the geology and any hazardous phenomena. If this was part of an assignment today he would get high marks on descriptions but not so much on sketches. At the beginning of each notebook he would also note down the adminstrative hierarchy (Governor, adminstrator, executive council etc.) and if he was accompanied by anyone. The most surprising find for me (and the most critical) was that he interviewed and gathered statements of those who observed volcanic activity. Reading these statements, another very important aspect became apparent, he was including more voices than the ‘white elite’ men. He spoke to black men and women whose voice I had so far not been able to read (granted he called them negroes and negresses but I guess that was the language at the time).
My most favourite statement, that I will share with you all, was from a surviour of a pyroclastic density current that flowed down the eastern flank of the volcano over the Orange Hill Estate House. People survived in a rum cellar, whilst a number died in the corridor leading to the cellar and the estate manager, his wife and nephew died on the verandah.
Statement of Taylor in one of Edmund’s field notebooks (AMNH: Box 3, Item 31)
Photograph of the Orange Hill Estate house (YM: TA123)
Cellar where survivors were found (YM: TA125)
“A cook told me that trash in front of cellar and some of the houses were set on fire by the hot stones. Taylor(who is a very intelligent black man) and the others said that the “cloud rolled down from the Soufriere along the ravines, struck the sea, burst into flames foof, foof, foof, and at once turned back toward the sugar factory striking the building with great force and forcing shut the heavy doors and the heavy wooden shutters of the window openings. Heat was very oppressive. Air suffocating. Smelled of sulphur (rotten eggs, one said). For four or five minutes it seemed as if everyone would die from suffocation and cries for water were heard on all sides. Then the air cleared a bit, though the rain of dust and stones continued”.
From all information gathered from my trip, I can understand the volcanic hazards better: what, where, when and their impacts. They will also help inform impacts on the agricultural and society, where possible.
I like to thank the Royal Geographical Society for funding.
It is now the 1st May, which means I have one month left here on St Vincent. I am starting to get a bit restless and want to come home to see my family and friends. But I can hold on for a little longer!
Reflecting back on my time here so far, I would say it has been character building, as well as a confidence booster. Some people say being in a different country for a while has a positive effect on people. I suppose I can agree with them.
Coming out here by myself as an independent PhD student has suited me fine, as I do prefer my own company. I have been away from distractions to really crack on with the data I aimed to collect here.
Doing a dissertation/thesis, whether undergrad, Masters or PhD, is really a lonely affair. Of course you have your supervisors and friends, but they are busy people are they not? Every project is different and the guidance from the supervisors vary, but for me, it has worked just fine. Although a part of me wishes at least one of my supervisors had the chance to come out here to experience this island for themselves!
The data collection here has been the utmost importance and confess, I have not had much time to rest. I would say on a weekend I have relaxed but, just yesterday I conducted more interviews. But, I did get to see a new part of the island. I went to the Mesopotamia Valley, a village called Belmont which lies on the ridges of an extinct volcano! It was an amazing view, beats the view of a Private School’s sports grounds back home.
The remainder of my time here will be getting the rest of my interviews done, then beginning to make scripts and code them.
Oh and it will be my birthday near the end of the month…so I have definitely decided to not work then and head over to the Grenadine island of Bequia. Can squeeze in a bit of holiday before this is all over.
All the way I wanted to try and frame myself like past adventurers who had climbed the volcano, so this entry is trying to capture the common themes in what has been written in the past.
Friday was an exciting day. I got to climb La Soufrière. Having a physical disability, it obviously made things difficult, but it has never stopped me doing what I wanted to do, and I think it makes reaching the top all the more rewarding for me. Especially the 12 hour sleep I had when I returned!
The expedition party consisted of secondary school students of two schools, one from Georgetown and the other Sandy Bay, officers from the Forestry department, members from NEMO, scientists from the Seismic Research Centre of the University of the West Indies, researchers from the STREVA project and also a number of locals from Kingstown and Park Hill.
The Montane rainforest looks like the volcano never erupted 37 years ago. Vegetation regrowth is rapid, the above description by Mr Benjamin Sharp, 78 years later, and the photos Dr Tempest Anderson took just after the May 1902 eruption and 5 years later, demonstrate that. Even after the 1979 eruption the same phenomenon occurs. It is very impressive, to see the volcano destroy life but then promote such healthy regrowth.
Can the same be said for the society? Well, time will tell from my studies and from others researching La Soufrière.
The path is a mixture of flat, leaf litter-covered paths, steady climbs, and muddy steep steps. After about half an hour or so, the first stop is “River Bed”, which is an area of prehistoric lava flows. There are big boulders, as well as small stones.
After the River Bed is a large number of steep steps that were certainly not made for my disability and little legs. I took my time though, saw some hummingbirds wiz around, so that was nice. After about another hour or more of steady climbing, the forest changes from tall, dense trees with an intense humidity, to shrub with plant and fruit species only found on La Soufrière. You can catch a nice refreshing breeze now too. An important thing however, is that with the absence of cloud, you can clearly see Georgetown, the principle town in the north Windward region. It looks small, and you can really feel the volcano dwarfing it.
The next and final stop before the summit is “Jacob’s Well”, another area of ancient lava and once upon a time, a place you could get fresh water, hence the name. This area is narrower than River Bed.
The last half an hour or so to the top was tough on me. It was mostly a steady slope, but luckily it was manageable. The nearer you get, the more loose rocks and ash you walk upon. Almost lost my footing a few times. I was one of the last to reach the top, people congratulated me to reaching it in one piece. Before I could catch my breath, someone said the crater is clear. I do not know where the energy came from, but I excitedly reached the edge.
And there is where I lost my breath.
I came across a diary of Special Magistrate John Anderson, who took the Leeward route to the summit in 1837. His feelings were, “Surprise, wonder and terror, strike the spectator at this majestic spectacle.” He also said the volcano was just as magnificent as The Vale of Chamouni in Switzerland, the first view of Geneva and the Alps, the Isle of Staffa, St Peter’s Church in Rome, the view of Edinburgh from Calton Hill, the Bay of Dublin and Menai Bridge in North Wales.
I don’t have such places to compare it to, but I agree with him. The sight is so majestic and such a thing of beauty. What you see, and looking down seeing the surrounding rich flora and fauna and Georgetown, does help to put the research in perspective though. This volcano is an agent of awesome and fearsome power, one third of the island can look up on a clear day and see it. They live around it. Villages, farms and everything else has been built on its volcanic deposits. Such things must be parallel with anyone who lives around or near an active volcano I am sure. The volcano is there, biding its time, while people just go about their business, with or without a second thought that there is something that can take everything away in a matter of days, hours, minutes or seconds.
On the way down, I unfortunately fell over three times. Got a bruise. But hey, no pain no gain right?
The secondary school students certainly had the energy and momentum I can only dream of having. But this volcano is more important to them than me. They need to see the volcano they live with up close, and no better way to learn about it than from the volcanologists and researchers who came along with them.
I’m still recovering from the trip but I can honestly say, every single muscle and joint that is hurting right now is 100 percent worth it.
“Altogether, this unparalleled scene must delight anyone alive to the Majesty of Nature. The Souffriere is a “Lion” which does not on inspection, belie its fame. I call to mind but few, which I have seen, that merit the same commendation. They are widely different in their characters, and the associations which they call up: – The Vale of Chamouni in Switzerland; – the first view of Geneva and the Alps, from the Jura Mountains, – the Isle of Staffa in the Hebrides; – Saint Peter’s Church at Rome, – Edinburgh form the Calton hill; the Bay of Dublin, – Menai Bridge; – and the Souffriere of St. Vincent, – will not suffer by familiar acquaintance. I cannot better describe the emotions excited by the first glance of this volcano, than by the recital of the following circumstance. A gentleman of my acquaintance ascended the mountain about 14 days after the last eruption. The soil was still warm, and every step told a fearful tale of horror. He was accompanied by a young Mulatto, who no sooner was brought to the brink of the abyss, than uttering a shriek, he dashed down the pathway, and terror smit, – never ceased his progress till he reached the strand at Wallibau, when he dashed into the waves, and swam to the vessel in which his Master had come down!”
Special Magistrate John Anderson, October 1837. In: McDonald R.A. (2001) Between slavery and freedom: special magistrate John Anderson’s journal of St Vincent during the apprenticeship. Philadelphia: University of Pennsylvania Press.