Publishing:Making Matter Lexicon/Embeddedness

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embeddedness

Femke Snelting

Embeddedness: a triple d word with tentacles in geology, surfacing every trouble possible from dependency to duress. There is nothing simple about this term: embeddedness means to be attentive to multiple inter-operating spacetimes, to resonate with what is below as well as with what is above and delà, to resist extraction, and to account for remote implications.[1]

In assembling ideas that are seemingly disconnected and uneven (the seabird and the epilogue, the song and the soil, the punch clock and the ecosystem, the streetlight
and the kick-on-beat), the logic
of knowing-to-prove is unsustainable because incongruity appears to be
offering atypical thinking.
Yet curiosity thrives.[2]

embeddedness:
to be set solidly into a mass

Ship merchants operating from the Liverpool docks in the nineteenth century needed the tides predicted and their clocks calibrated, so they commissioned the Bidston Observatory. The observatory was to be strategically situated on the highest point of the Wirral peninsula, overlooking the river Mersey, the river Dee, and the Irish sea. Completed in 1866, it was made out of sandstone extracted from the bedrock below, creating a cavity which now forms the observatories’ extensive basements.[3] Around the building, a deep moat was dug to minimize interference from neighbouring traffic. The plinth in the picture (p. 30) is a ‘bedrock connection point’, located in the observatory sub-vault. Sheltered from temperature shifts and movements from elsewhere, the plinth provided a stable platform for a century of exacting earth observation.


Cornwall, last fall. Suddenly they feel the ground tremble, and hear windows rattle. Afterwards, Dr. Ryan Law, managing director of Geothermal Engineering explains to the local press:

As part of the United Downs Deep Geothermal Power testing, we did cause some micro-seismicity. Although this was within our regulatory limits,

we are stopping operations until we understand the cause. The tremors are low-scale and should not be anything to be afraid of.[4]

Geothermal energy is produced by harnessing heat from the earth’s core. To produce power from this heat, extremely deep wells need to be drilled and water is pumped through them at high pressure. Since the Bronze age, Cornwall has been mined for tin, copper, arsenic, and lithium. Tremors in the porous underground are set off as a result of the additional disturbance caused by geothermal boring. In the non-committal words of the general manager, they sense all the troubles that wreck the earth: ‘we caused micro-seismicity’ ... ‘within our regulatory limits’ ... ‘until we understand the cause’ ... ‘not anything to be afraid of’.

© Kym Ward (2022).

embeddedness:
laying in a bed of surrounding matter

South or north of here, already more than ten years ago. It takes him many long days to level the driveway of his holiday home. Using a barre à mine, a forged iron bar originally used by miners to pound the ground and break the surface, his movements reverberate through the valley. Eventually, he hits an immovable piece of rock and the pounding stops. He points, almost proudly, and says: ‘look, the earth!’  

Early on, the observatory installed a seismometer on the sub-vault plinth. Kept in the dark, it continuously auto-registered slight movements on light sensitive paper that corresponded with earthquakes experienced on the other side of the planet. A Milne-Shaw Vertical Tiltmeter was acquired in 1910, a precision instrument based on the same principle as the seismograph, where one part remains stationary and fixed, while another part moves together with the earth’s surface. The vertical tiltmeter derives its precision from using a rigid arm that points upwards, with a pendulum hanging down from it. The swinging of the pendulum, with its fulcrum fixed to the bedrock connection point, makes micro-seismicity observable by magnifying the actual motion of the earth. It was with this instrument that the phenomena of ‘tidal load’ could be observed, the oscillating north-south tilt of the Wirral peninsula due to the strain of the water weighing down the bedrock (and subsequently, the plinth itself) at high tide.


A physiotherapist once told me about her interest in how bodies feel their way around with the help of instruments. She explained her fascination through the example of cooking a soup or a sauce. If you stir the bottom with a wooden spoon, she said, you will feel precisely at which moment it starts to catch. You do not need to put your hand into the hot liquid to touch the bottom of the pan.


At the observatory, the so-called ‘ocean loading effect’ continued to be registered with increased precision until the early seventies, when the expanding data about earth tides from around the world started to show unexplained discrepancies in neighbouring sites; the magnitude of the north-south tilt varied by twenty percent when measured in one end of its sub-vault, or the other. In an article called ‘Tidal Tilt Anomalies’, two scientists working at Bidston claimed that these inconsistencies could be explained by unknowable couplings between the landmass movement and the strain on the site itself. ‘A mine or a tunnel, in which tilt measurements are usually taken, represents a discontinuity in the Earth’s crust.’[5] By comparing different types of instruments, they found that tiltmeters were extremely accurate but that they were measuring tidal tilt in combination with hyper local movements due to situated geological conditions. Tidal tilt observations where eventually abandoned due to non-compliant embedded data.

embeddedness:
trembling with the earth

As with many material evidences of techno-scientific progress, the appointing of stability, the fixing of a point zero wherever convenient, seems to require an entitled mode of being in the world.

Each point is merely a conceptual marker, which can be assigned and reassigned in the equation hierarchy as the ‘coordinating zero point’ and every line can be formed to be the ‘coordinating axis’.[6]

Power arranges itself around such arbitrary vantage points, through which the movement of goods and people elsewhere can be controlled. Contributing to the reliable navigation of ships across the British empire, but also actively and continuously supporting the convenient fable of transparent observation, the Bidston Observatory aligned with different scales of capitalist endeavour, exploitation, colonialist and imperialist modes of worlding.[7]


He is being driven around his native island Martinique, pointing out the places that he grew up in and that vanished after the earthquakes. The island is part of an archipelago located on the crumbling intersection of two tectonic plates, which makes the geo-plasticity of the earth regularly interact with human activity. ‘We understand the world better if we tremble with it’, he explains.[8]

To be embedded depends politically nor epistemologically on a fixed locus of observation. It opposes systematic thinking without fear, because it is a mode of understanding the world that resonates with the multidimensional and multidirectional impact of being embedded, of its inherent instability. Embeddedness is to ‘tremble with the world’.

The image cuts back to the view from the car window, an undulating green landscape moving by under a bright blue sky filled with clouds. He continues:

The world trembles in every way. It trembles organically and geologically. It trembles even with the climate, poor me, as far
as I know. But the world also trembles through the relations
we have with each other.[9]

  1. This contribution is based on the script for a performative introduction to the sub-vault of the Bidston Observatory Artistic Research Centre (BOARC) for participants of the work session Down Dwars Delà, organized by Constant and BOARC, Liverpool, August 2021, constantvzw.org/site/Open-call-study-session-Down-Dwars-Dela-2-UK.
  2. Katherine McKitttrick, Dear Science and Other Stories (Durham: Duke University Press, 2021), p. 4.
  3. The Bidston Observatory was built on the solid bedrock of the Wirral peninsula, ‘a capping of Keuper sandstone on soft Upper Bunter’, which was considered to be more stable than other geological arrangements elsewhere. Joyce Scoffield, Bidston Observatory: The Place and the People (Merseyside: Countyvise Ltd, 2006).
  4. Sabi Phagura, ‘Houses shake as Cornwall is rocked by FIFTEEN “earthquakes” measuring up to 1.5 in magnitude in two days caused by tests at geothermal drilling site’, Daily Mail, 1 October 2020, dailymail.co.uk/news/article-8794885/Houses-shake-Cornwall-rocked-15-earthquakes-two-days.html.
  5. T.F. Baker and G.W. Lennon, ‘Tidal Tilt Anomalies’, Nature 243 (1973), pp. 75–76.
  6. Clancy Wilmott, Mobile Mapping Space: Cartography and the Digital (Amsterdam: Amsterdam University Press, 2020).
  7. ‘The Center is Open/HECS is ajar!’, wiki.bidstonobservatory.org/index.php/About.
  8. Manthia Diawara, ‘One World in Relation: Édouard Glissant in Conversation with Manthia Diawara’, NKA Journal of Contemporary African Art 28 (Spring 2011), pp. 4–19.
  9. Ibid.