New England's History

Discussions on the history and historiography of Australia's New England

Monday, June 16, 2025

Arabian Peninsula Wet Periods - a note

 My last note discussed Marine isotype Stages (MIS). These provided a dated measurement of glacial (dry climate) and interglacial (wetter) periods over extended time periods. The most relevant time periods from our perspective are summarised below 

"MIS 4 – 71

MIS 5 – 130, usually sub-divided into a to e:

MIS 5a – 82 (peak of interglacial sub-stage)

MIS 5b – 87 (peak of glacial sub-stage)

MIS 5c – 96 (peak of interglacial sub-stage)

MIS 5d – 109 (peak of glacial sub-stage)

MIS 5e – 123 (peak of Last Interglacial, also known as the Eemian among other names)

MIS 6 – 191 (Penultimate Glacial Period, also called Illinoian glacial in North America, later Saalian in northern Europe and later Wolstonian in Britain)

MIS 7 – 243 (Aveley Interglacial in Britain)"

If the Aboriginal ancestors came out of Africa they would have had to travel through the Arabian Peninsula. But was that possible? The work of Abi Stone et al (2023) suggest that it was.

Abstract:

"Past environmental and climatic conditions within the Arabian Peninsula are key to understanding the setting for hominin dispersal across the Saharo-Arabian dryland belt. The tufa deposits within the volcanic harrats on the southwest coast of Saudi Arabia fill a significant spatial gap in the distribution of palaeoenvironmental records on the west coast of the Arabian Peninsula adjacent to the Red Sea. In the catchment of Wadi Dabsa in the Harrat Al Birk, there are widespread fossil palustrine to shallow-lacustrine tufa deposits with fluvial elements. Several phases of tufa accumulation, separated by fluvial downcutting, are observable within these powerful palaeoenvironmental proxies. U–Th dating of targeted dense, banded tufa facies, yield ages that are stratigraphically consistent at the landscape scale, and indicate that tufa accumulation occurred during distinct humid phases broadly coeval with the last two warm interglacial Marine Isotope Stages (MIS 7 and MIS 5). For the first time this shows humid intervals in southwest Arabia coincident with the southern coast. There is a similar pattern emerging further north in the Arabian Peninsula, The Sinai and Levant and further on into continental Europe. Furthermore, tufa δ18O ranges from −14.6 to −1.9‰, covering a range similar to those reported for tufa from north African oasis sites and speleothems elsewhere on the Arabian Peninsula and The Levant. The lowest δ18O values are derived from MIS 5e samples, a pattern in agreement with speleothems in Yemen and Oman, and consistent with an isotopic-enabled climate model simulation for this time slice. The δ13C and Sr isotopic compositions of dated tufa samples indicate deposition from shallow-circulating meteoric water, with no geothermal influence. This, along with the δ18O values, suggest a freshwater supply that was a potable water source in this landscape. The δ13C signatures at Wadi Dabsa are more negative than for parts of north Africa, suggesting Wadi Dabsa may have experienced comparatively higher biomass, thicker soils and wetter conditions with lower evaporative losses. This new record of tufa deposition during the middle and late Pleistocene, suggests for the first time that the west coast of Arabia experienced a similar history of humid phases over the past 250 ka as southern Arabia and the Nefud in the northern interior. These regional changes in hydroclimatic regime occur at timescales coincident with hominin dispersals." Abi Stone, Robyn H. Inglis, Ian Candy, Diana Sahy, Anne-Lise Jourdan, Dan N. Barfod, Abdullah M. Alsharekh, “Humid phases on the southwestern Arabian Peninsula are consistent with the last two interglacials”, Quaternary Science Reviews, Volume 319, 2023, https://doi.org/10.1016/j.quascirev.2023.108333 

Comment

The warmer wet periods suggested by the analysis do appear to fit with an out of Africa date of 72000 kya (MIS 5). An earlier date might also be possible to fit with MIS 7 should the present latest date for occupation within Sahul (c65,000 kya) be pushed back. 

 

Thursday, June 12, 2025

Marine Isotype Stages - a note

 DNA analysis suggests that the descendants of Australia's Aboriginal peoples left Africa perhaps 72,000 years ago. To reach Australia they would have travelled through the Arabian Peninsula. This is a desert area today, difficult to traverse. But was this always so? Were there periods when  the Peninsula was green in whole or part, when the Aboriginal ancestors might have passed? 

A clue here might be provided by Marine isotype stages (MIS). The material that follows is drawn from Wikipedia. 

What are Marine isotype stages?

Quoting:

"Marine isotope stages (MIS), marine oxygen-isotope stages, or oxygen isotope stages (OIS), are alternating warm and cool periods in the Earth's paleoclimate, deduced from oxygen isotope data derived from deep sea core samples. Working backwards from the present, which is MIS 1 in the scale, stages with even numbers have high levels of oxygen-18 and represent cold glacial periods, while the odd-numbered stages are lows in the oxygen-18 figures, representing warm interglacial intervals. The data are derived from pollen and foraminifera (plankton) remains in drilled marine sediment cores, sapropels, and other data that reflect historic climate; these are called proxies."

 The Stages


The following represents the dates etc of some of the stages most relevant to my topic.

Quoting

"The following are the start dates (apart from MIS 5 sub-stages) of the most recent MIS (Lisiecki & Raymo 2005, LR04 Benthic Stack). The figures, in thousands of years ago, are from Lisiecki's website.[13] Numbers for substages in MIS 5 denote peaks of substages rather than boundaries.

MIS     Start date
MIS 1 – 14 kya, end of the Younger Dryas marks the start of the Holocene. The LR04 date of 14 kya had to accommodate less well studied time intervals, and the generally accepted date of 11.7 kya is to be preferred.[14]
MIS 2 – 29 (Last Glacial Maximum)
MIS 3 – 57[a] (MIS 2-4 is called the Last Glacial Period, Wisconsinan glaciation in North America, Weichselian glaciation in northern Europe)
MIS 4 – 71
MIS 5 – 130, usually sub-divided into a to e:
MIS 5a – 82 (peak of interglacial sub-stage)
MIS 5b – 87 (peak of glacial sub-stage)
MIS 5c – 96 (peak of interglacial sub-stage)
MIS 5d – 109 (peak of glacial sub-stage)
MIS 5e – 123 (peak of Last Interglacial, also known as the Eemian among other names)
MIS 6 – 191 (Penultimate Glacial Period, also called Illinoian glacial in North America, later Saalian in northern Europe and later Wolstonian in Britain)
MIS 7 – 243 (Aveley Interglacial in Britain)
MIS 8 – 300 (early Wolstonian in Britain)
MIS 9 – 337 (Purfleet Interglacial in Britain)[16]
MIS 10 – 374
MIS 11 – 424 (Hoxnian Interglacial in Britain, and Holstein Interglacial in Central Europe)"

Comment

If you look at the stages you will see that MIS 4 and 5 are the most relevant to our story. In my next note I will move from the broad stages to look at some of the research relating to the Arabian peninsula to check when the Aboriginal ancestors might have been able to come. 

Saturday, May 31, 2025

Immediate priorities in the writing of New England's history - Aboriginal New England to 1788: Origins

 My present first priority in completing my history of Australia's New England is the creation of a full working draft for the history of New England's Aboriginal peoples to 1788 starting with origins and journey.  Where and when did their ancestors come from? How did they get to Sahul? Who did they mix with on the way? When did they arrive in the area that I call New England? How did they get there?

I covered this material in my lecture series to Armidale U3A but now need to consolidate and update it. Power points are a real trap here. A set of summary power points does not a history make! I had become very dissatisfied with my work but then realised that was silly. I am presenting a story, really a series of hypotheses linked to create a synthesis. No matter how much time I spend there will always be errors of fact and interpretation. Better to get it out there so that it can be critiqued, recognising that the pace of new discoveries will quickly over-run my analysis.  


  

Friday, May 30, 2025

Belated Blogging update 30 May 2025

 While personal circumstances have limited all my research and writing activities, I have kept this blog open to allow for comments on past posts since it is clear that people are still reading it and commenting. Since my last post on 7 November 2023 there have been dozens of such comments excluding the inevitable spam, many on posts from early in the blog's history. Together, they constitute quite a valuable resource. 

 Some months ago I returned to research and writing (and book buying!) focused on my main history projects. This was mildly depressing at two levels: I found more gaps in my research, while there had been a mass of new material published that I needed to take into account! Still, I am now at the stage where I feel the need to revive this blog. Hopefully I can do this in a productive way.   

Tuesday, November 07, 2023

Introducing the Museum of Stone Tools - an invaluable resource

 


One of the challenges in teaching the history of Australia's New England over such a long period lies in the sheer range of topics and disciplines that need to be included. One example is the stone artifacts that formed key elements in Aboriginal toolkits. 

Uniface pebble chopper tools from the Seeland's dig, Clarence Valley

From these surviving physical manifestations we can deduce something about the changing patterns of life over time, about the relationship between the Aborigines and their environments, about trade and the relationships between Aboriginal groups.

I started with some base knowledge in this area. Back in the 1960s I was a student member of Isabel McBryde’s pioneering UNE prehistory group. My second paying job during University vacations was as a research assistant for Isabel sorting, classifying and recording stone tools. However, in 2020 when I came integrate Aboriginal tools into my story of Aboriginal New England to 1788, part of my broader course on New England’s history to 1788, the gaps in my knowledge quickly became clear. 


The 2020 course was badly affected by the covid epidemic. However, one plus of the epidemic and its shutdowns is that it led UNE’s Professor Mark Moore to begin the development of the on-line Museum of Stone Tools. Mark is one of Australia’s leading archaeologists and an expert in stone flaking techniques. 

Professor Mark Moore

The resulting museum provides examples of various stone tools from across the world supported by explanatory material. Central to it are 3D models that allow you to play with various implements rotating them as required. The overall analysis is simple and accessible designed for people of all ages. You do not need specialist knowledge to understand. 

I hope to run my course again in the second half of next year. I think that the museum will prove a real blessing. In the meantime, do have a browse.


Monday, October 10, 2022

The impact of periodic drought on Aboriginal life and history - a note

Interesting piece in The Conversation (6 October) by Kathryn Allen, Alison O'Donnell, Benjamin I. Cook, Jonathan Palmer and Pauline Grierson, "Megadroughts helped topple ancient empires. We’ve found their traces in Australia’s past, and expect more to come".  The article includes a link to a 2016 paper that I had not seen that attempts to construct  a 1013 year rainfall chart for the Williams River in the Hunter Valley - Carly R. Tozer, Tessa R. Vance, Jason L. Roberts, Anthony S. Kiem, Mark A. J. Curran and Andrew D. Moy, "An ice core derived 1013-year catchment-scale annual rainfall reconstruction in subtropical eastern Australia", Hydrol. Earth Syst. Sci., 20, 1703–1717, 2016, www.hydrol-earth-syst-sci.net/20/1703/2016/ doi:10.5194/hess-20-1703-2016.

Attempts to reconstruct Aboriginal history over the long period of human occupation of Sahul then the later Australian continent including my own for the broader New England tend to focus on broader trends such as the impact of the Last Glacial Maximum and the subsequent emergence of the Holocene. While this is inevitable,  it is easy to ignore the significant impact on Aboriginal life of major changes within periods including long mega droughts and subsequent wet periods. 

If we take the Murray River as an example, I'm working from memory here, Mulvaney notes the evidence of periodic malnutrition in skeletal remains. Here we have relatively small territories with substantial populations dependent upon drought exposed riverine resources. On New England's western slopes and plains the pattern of life seems clearly affected by periodic droughts. 

I haven't worked all this through. For the moment, this is just a note for further thought.  

Tuesday, October 04, 2022

Taree's first eisteddfod, 1913

The Kurri Kurri choir who won the chief choral contest at the 1913 Taree eisteddfod (Photo  MidCoast Stories via the ABC)
Interesting piece by the ABC's Emma Siossian, Taree's first eisteddfod in 1913 was an impressive feat of logistics and planning.

As Heritage website  MidCoast Stories co-founder Penny Teerman noted, music festivals were popular in the early 20th century. In 1912, a limited but successful festival was held in Taree. This provided the impetus the following year for the formation of the Manning River Musical Festival Society - Penny calls it the Taree Musical Society but Trove searches suggest that it had a broader title  - to put on a larger event with multiple activities. This was a considerable success with multiple performers and a large number of spectators. 

The Leichhardt Boy's Choir performed in Taree during 1913..(Photo  MidCoast Stories via ABC)

I will leave you to read the story but wanted to make a few comments from my perspective as an historian of the broader New England. 

I was not sure about the use of the word eisteddfod. I think that the first named eisteddfod was put on in Ballarat in 1855 by Welsh miners attracted to the new gold fields, but widespread use of the name as opposed to musical festivals came later. I checked Trove, and the name eisteddfod was indeed used

Transport difficulties limited the scope of major events. On the North Coast where river transport was possible, events would draw along river routes. As the railways spread, they provided a means of drawing in a broader audience or group of participants. The 1913 Taree eisteddfod followed the opening of the railway. Participation still focused on surrounding areas but broader participation was possible, We can see this in 1913: participants came from regional areas linked by the railway but participation from the more distant Leichardt Boys Choir was also possible if more expensive

I noted the Kurri Kurri Choir. Music was an important form of shared entertainment on the coal fields. The number of attendees at band performances is a sign of just how popular local band music was.  

Tuesday, August 30, 2022

New DNA studies provide new light on the mixing of people in the classical world

 Interesting piece by Andrew Curry in Science, "‘Phenomenal’ ancient DNA data set provides clues to origin of farming and early languages: Trio of studies suggests new homeland for earliest Indo-European speakers and traces movements of ancient Greeks, Imperial Romans". The story includes links to related stories. 

I'm not quite sure how to interpret the material, but it does show (again!) how genomics is throwing new light on evidence revealed via the archaeological record.  

Friday, January 21, 2022

Callum Clayton-Dixon’s Surviving New England

As my first post for the new year, I am publishing the book review originally published in the Armidale and District Historical Society Journal in October last year. I am publishing it here because the Journal is not on-line. Callum's book deals with the frontier warfare period on the New England Tablelands. 

I think that's it's an important book written from an Aboriginal perspective focused on the Aborigines as people with agency. These stories need to be told at regional level. If we examine Callum's work with other studies such as Mark Dunn's Convict Valley we have a much better chance of building a coherent story that includes inter-regional interactions. I wish someone would do a similar study of the North Coast.   

Book Review: Callum Clayton-Dixon’s Surviving New England

Callum Clayton-Dixon’s Surviving New England: A history of Aboriginal resistance and resilience through the first forty years of the colonial apocalypse[i] is an important book, although some find it discomforting.

Clearly and simply written, the book discuses  the impact of European occupation on the life of the Aboriginal peoples living on Australia’s New England Tablelands from the 1830s into the 1860s. In doing so, it focuses on the Aboriginal experience in a particular area at a critical point in time.

Background: the importance of regional studies

We sometimes talk of the “Australian Aborigines” as though they were and are a single entity. We know that this is not true, but the habit lingers, affecting the way we approach both policy development and historical analysis.

We now know that the Aboriginal and Papuan ancestors arrived on the mega-continent we now call Sahul perhaps 65,000 years ago. This was the Pleistocene, a geological epoch marked by recurrent ice ages during which sea levels fell and rose as the ice advanced and retreated. With lower sea levels, Papua-New Guinea, the current Australian continent, Tasmania and much of the continental shelf were joined in a single great continent. 

By 42,000 to 40,000 years ago, all of Sahul from the Papuan Islands in the north to Tasmania in the south had been at least lightly occupied. Around 21,000 years ago a cold and desolate period known as the Last Glacial Maximum began. Sea levels fell to perhaps 130 metres below present levels, temperatures fell dramatically on land and in the sea, rainfalls declined sharply.  This forced the Aboriginal ancestors to retreat and regroup and may have threatened the very existence of human occupation of Sahul.

Around 15,000 years ago a warmer period known as the Holocene began, As the glaciers melted, the seas rushed back separating Papua and Tasmania from the Sahul mainland, submerging large areas of the continental shelf. This period is recorded in Aboriginal folk lore referencing great floods.

By 1788, a complex Aboriginal society had emerged across the new Australian continent. This society was not uniform, but varied from area to area in culture and relationships with the landscape. This society would now be torn apart, a process that varied across space and time depending on the spread of European settlement, local conditions and the policies of the emerging colonial jurisdictions.

I make these points because a proper understanding of our history and especially Aboriginal history requires a focus on local and regional experiences.

As I read Callum’s book, I thought just how well it fitted into the New England historiography tradition. 

Both the Armidale Teachers’ College (later the Armidale College of Advanced Education) and the New England University College (now the University of New England, UNE) were founded in part to study and preserve the history and culture of Northern NSW, the North.

When Isabel McBryde came to Armidale in 1960, she was the first tenured Australian university staff member to have the word prehistory in her title. The students she recruited to study the ethnography and prehistory of the broader New England would form the first archaeology and prehistory honours class in Australia,

From the beginning and under the influence of her mentor John Mulvaney, Isabel focused on the creation of a regional historical sequence. She and John believed that the variety in Aboriginal culture and society meant that you could not understand the history without a focus on regional studies. In parallel, the English Department’s Bill Hoddinott began the documentation of Aboriginal languages within Northern NSW.

In 1962, Robin Walker published an article discussing the relations between Aborigines and settlers in New England 1818-1910.[ii]  

In 1966, two years before W E H Stanner coined the phrase the Great Australian Silence to describe the absence of Aboriginal history in Australian history, Walker published Old New England, a history of the Northern Tablelands from 1818 to 1900.[iii] While Walker focused on the settler experience, the book begins with an outline of Aboriginal life prior to European occupation. Later, it explicitly recognises the existence of frontier warfare including massacres and retaliatory killings and the damage done to Aboriginal society as a consequence of disease and disruption.

In 1981, Geoff Blomfield published the first edition of Baal Belbora: The End of the Dancing[iv], a study of warfare, massacres and frontier violence in the Falls’ country of Southern New England.

Callum’s Perspective

These few examples suggest the importance of regional studies, as well as showing early recognition of both frontier warfare and the impact of European occupation on Aboriginal society. However, they were all written by non-Aboriginal people.

Callum writes from an Aboriginal perspective. His focus is more personal, more political. It centres on the Aborigines as people with agency, people who responded to invasion by fighting back against overwhelming odds.

This is a very different perspective from the sometimes simple minded focus on the Aborigines as victims. To Callum, his ancestors were warriors who in the end survived. In writing, he seeks to instil pride in an often oppressed group.  

 Callum’s position is clearly set out the book’s Introduction. It begins with his discovery of his Aboriginal ancestry, of his return to the country of his ancestors, of his attempt to discover and reconnect with country.

Callum writes from a particular post-colonial mental structure. As Callum discovered his own past, he became involved with groups such as the Warriors of the Aboriginal Resistance who were determined to tear down the mental, social and legal barriers that prevented proper recognition and reconstruction, the reinstatement of the rights of all the Aboriginal peoples.

Callum’s position is not limited to Australia’s Aboriginal peoples, but indigenous peoples everywhere. To his mind, justice demands the deconstruction of structures created by colonialism and their replacement by new structures that properly recognise indigenous ownership and rights.

This approach could leave him open to the charge that his book is a polemic, a political statement, rather than a piece of historical research. That would be unjust. This is good history. I say this for several reasons.

All historians write from particular perspectives. This affects the questions they ask and evidence selected. Often, these positions have to be inferred. By contrast, Callum tells us where he is coming from. We can therefore make our own judgements on approach and evidence presented. Here Callum has been careful to document his evidence, allowing us to follow up, to check his sources and again form our own views.

A mark of good history is the extent to which it provides insights that allow us to see patterns, to develop new ideas. Callum’s book passes this test.

Setting the Scene

Having outlined his personal position, Callum discusses key questions that set a framework for the following story of resistance. What was the Aboriginal population of the Tablelands at the time of British occupation? How rapidly did occupation proceed? What was the impact of British occupation on the Aboriginal peoples and population?

 When I made the first estimates of the distribution of Aboriginal populations across Northern NSW, I worked (as Callum does) from settler and official records.[v] In doing so, I was unaware of the impact of diseases such as smallpox, influenza, measles and venereal infections that spread far beyond the moving frontier. This affected population size directly through deaths and then through reduced fertility rates within surviving populations.

Taking this into account, Callum estimates the Tablelands’ population as between 1,100 and 1,200 people. Accepting that the Tablelands were not as productive in Aboriginal terms as the coast and western slopes and immediate plains, I suspect that this is an underestimate. I say this because the number of recorded languages and their supporting dialects, the number of recorded Aboriginal groups, is quite high. A simple division of these numbers into the population estimates gives figures too small to be viable units in demographic terms.

Perhaps wisely given the population uncertainties, Callum does not attempt to scope the number of warriors (men of fighting age) at the time of European occupation. This is an important issue because it helps scope the scale of the conflict that followed. If we exclude women, children and older men, a population of 1,200 suggests perhaps 400 warriors spread across multiple local groups.

Using graphs, Callum charts the rapid growth of the settler population across the New England Tablelands from 1830 to 1850. European occupation began in the early 1830s with the squatters coming in two streams, one inland from the Hunter, the second from Port Macquarie where Archibald Clunes Innes had established his headquarters.

This expansion was driven by demand for the wool required to feed the growing British textile industry. It was also driven by a speculative fever as the new settlers sought to build their fortunes.

The New England Tablelands may have been a relatively poor territory in Aboriginal terms, but it was well suited to wool growing. The result was a settlement explosion.  By the time Crown Lands Commissioner Macdonald established his headquarters in 1839 at the place now called Armidale, much of the New England was at least lightly occupied. By 1841, the European population had reached 1,115, rising to 2,231 in 1846. The Aborigines were now in a minority. The effect is more pronounced still if we consider the male population, for in this period there were few women in the European population. This meant that the number of European men of what we might call military age outnumbered the number of Aboriginal warriors well before the European population outnumbered the Aboriginal population. 

Patterns of Aboriginal Resistance

European expansion had devastating effects on Aboriginal traditional life. Beyond the effects of disease, beyond losses in frontier warfare, came the effects associated with destruction of habitat as the Aboriginal peoples were denied access to the traditional lands, forced to retreat to marginal areas. Callum calls this process ecocide, the sometimes deliberate destruction of the economy and environment on which a people depends for their survival.

Callum explores the Aboriginal response in a number of chapters plus an appendix that lists all the examples of frontier violence that he has found from the records as well as Aboriginal memories, some 41 items in all. Unlike the University of Newcastle’s Colonial massacres project which focuses on specifically defined massacres[vi], Callum’s focus on the Aboriginal response means that he is as interested in all types of Aboriginal response against the European invasion.

I think that this is very important in opening new areas of historical analysis, although I think that there are weaknesses in Callum’s analysis, areas that he does not address.

This may sound like a criticism. It is not. Callum has proven his basic point, that the Aboriginal peoples were people with agency who fought back. He has opened new ground for historical research, new questions and structures that I find interesting. He and we can build on his research to tell new stories.

To extend my argument, using Callum’s structure we can think of the Aboriginal response in terms of three phases, sometimes uneasy co-existence, resistance and then survival. We can also think of this in terms of the structure of Aboriginal society, the structure of European colonial society and the way the two played out in the pattern of frontier life. We can also think of this in regional and local terms. Here we can learn much from other regional studies such as Mark Dunn’s The Convict Valley, the story of early European settlement on the Hunter[vii].These regional studies allow us to learn much about different patterns over space and time, but also allow us to see interconnections between different areas.

If you look at the patterns of early Aboriginal resistance, they included attacks on isolated individuals with attacks on stock. The Aborigines were selective in such attacks, focusing on individuals who had done them wrong. As resistance gathered strength, you had large scale attacks on people and stock.

In both the Hunter and on the New England, the European response forced Aboriginal groups to the more remote and rugged country where horses could not easily penetrate. There different Aboriginal groups came together to mount larger scale attacks on people and stock. On the New England, for example, growing European settlement on the coast seems to have forced coastal Aborigines to the west where they joined with Tablelands’ groups including traditional enemies to mount large scale attacks. The patterns created last to this day.

The exact patterns including regional linkages are poorly understood. As Callum notes, he had to develop his synthesis from a variety of often fragmented early settler and official records, records written from the other side of the conflict.

Reading Callum’s work in conjunction with other studies such as Mark’s. I thought that there that there is so much more that we might say. We will never know of course, we have to infer so much, but Callum’s work gives us another block to build from.

Publication Details:

Jim Belshaw, “Book Review: Surviving New England”, Armidale and District Historical Society Journal and Proceedings, No 64, October 2021, pp 102-106



[i]  Callum Clayton-Dixson, Surviving New England, Aniawan Language Revival Program, Armidale 2019. Reprinted NEWARA Aboriginal Corporation, Armidale 2020

[ii] R B Walker,  ‘The Relations between Aborigines and Settlers in New England 1818-1900, Armidale and District Historical Society Journal, 4, 1962 pp1-18

[iii] R B Walker,  Old New England: A history of the Northern Tablelands of New South Wales 1818-1900, Sydney University Press, 1966

[iv] Geoff Blomfield,  Baal Belbora: The End of the Dancing, Apcol, 1981

[v] Jim Belshaw, The Economic Basis of Aboriginal Life in Northern New South Wales in the Nineteenth Century, BA Hons thesis, University of New England, 1966; J Belshaw, ‘Population distribution and the pattern of seasonal movement in northern New South Wales’, in Records of Times Past, I McBryde (ed.). Australian Institute of Aboriginal Studies, Canberra: 1978, pp.65-81

[vi] Colonial Frontier Massacres in Australia, 1788-1930, University of Newcastle, https://c21ch.newcastle.edu.au/colonialmassacres/

[vii] Mark Dunn The Convict Valley The bloody struggle on Australia's early frontier Allen & Unwin June 2020


Saturday, December 04, 2021

The fall of Archibald Clunes Innes

In 1840, Port Macquarie’s Archibald Clunes Innes was at the height of his wealth and power with stores, pastoral runs and real estate holdings on the coast and across the New England. Now he faced economic storms of cyclonic proportions.   

Opposition to transportation had been rising, driven in part by the growing number of free workers especially in Sydney who saw the convicts as an economic threat, in part by those who believed that continued transportation was incompatible with the development of a free colony.


Aberglasslyn House outside Maitland is an example of the rise and falls associated with the crash of the early 1840s. This monumental Georgian pile designed by architect John Verge for George Hobler, remained unfinished following Hoblers insolvency in the crash.

In face of protests, transportation to NSW was suspended in 1840. Innes had built his wealth in part on access to convict labour to service his growing empire. Now he and other squatters faced labour shortages together with rising wage costs, leading to a search for new workers.

 Later in the decade, this would bring the first Chinese and German workers to New England, but the initial effects were severe. However, these were the least of Innes’s problems.

Over the 1820s and 1830s NSW experienced a sustained economic boom.

High wool prices fueled pastoral expansion which in turn inflated stock prices. The previously small European population grew from 7,040 in 1807 to 28,024 in 1820, to over 44,000 in 1830, passing 127,000 in 1847, inflating real estate prices. Land sales inflated Government revenues that were used in part to fund immigration.

 Growth required capital drawn heavily from English investors and the London capital market, fueling the growing boom. Fortunes were being made from speculation in stock and real estate, fortunes invested in further speculation and in the construction of the first grand homes including Lake Innes House. Now all this came to a shuddering halt.  

 In 1837, a speculation fueled US boom part fueled by English capital crashed. This led to a financial crisis in England in 1839, drying up the capital that had been fueling the NSW boom.

Wool prices dropped sharply as did live stock prices, a fall accentuated by the ending of the rapid pastoral expansion that had driven up prices as stock was purchased to stock the new runs. Government revenues from land sales fell sharply, creating a Government financial crisis.

The end result was a rolling series of bankruptcies among those who most exposed to the boom including that of merchant, pastoralist and steamship owner Joseph Grose in 1844. Grose’s spread of interests made him a considerable figure in the early colonial history of Northern NSW’

 Innes could not escape the turmoil. Initially he seems to have refinanced his operations using family money. But then, in 1843, the collapse of a large Sydney based pastoral house led to the collapse of a major local bank that would finally force Innes into bankruptcy. An era had ended.