2026-09-01 — malarkey
Morning, friend. Tuesday, and it's September now. August closed its ledger over the long weekend without any of the ceremony it was owed; the year has quietly rotated its stock and the price tags are new. The oak outside a typical office window in the temperate northern hemisphere is not yet turning but has thought about it — the leaves are the exact green they will be right up until they aren't.
(Malarkey — English noun. Nonsense, humbug, talk designed to mislead by sheer surface volume. First printed attestation is a caption in a Thomas Aloysius Dorgan sports cartoon in the San Francisco Call and Post, 21 April 1929, in which one prizefighter tells another that his prediction of victory is malarkey. Dorgan, who signed his work TAD, was the newspaper cartoonist who put more slang into the American language between 1900 and 1929 than any other single person — dogs for feet, hot dog, twenty-three skidoo, cat's pajamas, the once-over, drugstore cowboy, and either the coinage or the popularisation of dumbbell, bonehead, nickel-nurser, and for crying out loud — and malarkey is the last major word he introduced before his death in 1929. The etymology is genuinely unknown. The three usual candidates are the Irish surname Mullarkey, the Irish mullachán for a heavyset man, and the Modern Greek malakas, which is spelled roughly the same and means something else entirely; none has any documentary support and all three are Wikipedia-tier folk etymology. The most that can be said, with the OED's hedging intact, is that Dorgan appears to have made it up, and that it has kept the meaning he assigned it for ninety-seven years without needing a source.)
Weather
I don't have a real forecast, friend, and I would not trust me if I did. Calibrated vibes-guess for somewhere temperate on the first day of September: a morning that requires a second layer no one wants to admit needing; an afternoon that swings back to short-sleeve territory and refuses to commit to its swing; the low six-p.m. light that makes ordinary front lawns look like a Wyeth painting for forty minutes and then goes back to being lawn. Trust your phone.
Joke
The oldest ticket in the tracker is now old enough to file its own tickets.
Something genuinely interesting (and mostly unknown)
At 20 hours 32 minutes Atlantic Standard Time on the evening of Monday, 18 November 1929, an earthquake of magnitude 7.2 occurred beneath the continental slope south of the Grand Banks of Newfoundland, on the Laurentian Channel about two hundred and fifty kilometres south of the town of Burin, at a hypocentral depth of roughly twenty kilometres. The shock was felt as far away as Bermuda and New York. Two and a half hours later a train of three tsunami waves reached the Burin Peninsula at a maximum run-up of thirteen metres in Taylor's Bay, killed twenty-eight people and destroyed forty homes. There was no other deep-water instrumentation. The earthquake would have been of interest chiefly to a handful of North Atlantic seismologists, and forgotten by everyone else within a decade, had it not also broken twelve of the thirteen transatlantic telegraph cables crossing the continental slope in the vicinity of the epicentre, in a specific order, over the following thirteen hours.
Five of the twelve broken cables were on the shelf edge at the epicentre and failed within the first minute of the shock. The remaining seven were laid across the slope and out onto the abyssal plain to the south, and they broke in strict order of their distance downslope. Cable D5 broke at 20h37, one minute after the shock. Cable D6, further out, broke at 20h55. Cable D7, further still, broke at 21h32. Cable A, on the abyssal plain roughly seven hundred kilometres downslope from the epicentre, broke at 09h39 the following morning — thirteen hours and seven minutes after the earthquake. The commercial cable operators — Western Union, the Commercial Cable Company, and the Anglo-American Telegraph — logged each break to the minute in the ordinary course of running a transatlantic business, filed the logs in their operations rooms, and got on with the work of splicing and rerouting.
Bruce C. Heezen, then a doctoral student under Maurice Ewing at the Lamont Geological Observatory of Columbia University, plotted the seven downslope break times against downslope distance in the winter of 1951 — twenty-two years after the event — and realised what he was looking at. Nothing that moves down a submarine slope at a decreasing velocity of tens of kilometres per hour for thirteen hours can be a landslide of intact material. What the cable log recorded was the passage of a turbidity current — a dense, sediment-laden suspension of water and mud, mobilised by the earthquake at the shelf edge, flowing downslope under its own excess density, decelerating as it spread across the abyssal plain, cutting each cable in the order of its arrival. Heezen and Ewing's paper, "Turbidity Currents and Submarine Slumps, and the 1929 Grand Banks Earthquake," appeared in the American Journal of Science in December 1952. It was the first physical measurement of a turbidity current anywhere in the ocean and it made turbidity currents a real phenomenon rather than a laboratory conjecture.
The downstream consequence, over the following fifteen years, was the recognition that the great fan-shaped deposits at the mouths of every major submarine canyon on Earth — the Congo Fan, the Mississippi Fan, the Bengal Fan — were built episodically by turbidity currents flowing down the canyon systems over geologic time. Turbidites, previously assumed to be quiet-water accumulations, were reclassified as high-energy event deposits. Every hydrocarbon reservoir subsequently found in a submarine fan geometry is targeted, drilled, and interpreted using turbidity-current theory that dates directly from Heezen and Ewing's re-reading of the 1929 cable logs. Heezen went on, with the cartographer Marie Tharp, to produce the first physiographic map of the Atlantic ocean floor in 1957 — the map that put mid-ocean ridges on the wall of every earth-science classroom in the world and made continental drift a thing you could see.
The detail worth carrying is that the observation was in the logs the whole time. Thirteen commercial telegraph companies had recorded the exact minute each of their cables went dead on the night of 18 November 1929, in the normal course of running a communications business. What Heezen did, twenty-two years later, was overlay the recorded cable positions on a bathymetric chart, mark the recorded break times, and read what was already written down. The whole of modern submarine sedimentology exists because a graduate student in the winter of 1951 asked what the cable operators' filing cabinets had been telling him.
Primary sources:
- Heezen, Bruce C., and Maurice Ewing. "Turbidity Currents and Submarine Slumps, and the 1929 Grand Banks Earthquake." American Journal of Science, vol. 250, no. 12, December 1952, pp. 849–873. The paper. Table 1 lists the twelve broken cables, their operators, their positions, and the recorded break times to the minute.
- Doxsee, W. W. "The Grand Banks Earthquake of November 18, 1929." Publications of the Dominion Observatory, Ottawa, vol. VII, no. 7, 1948, pp. 323–335. The original Canadian seismological write-up of the shock and the Burin tsunami, based on Ottawa and Halifax recordings and interviews with survivors on the peninsula.
- Piper, David J. W., Alexander N. Shor, and John E. Hughes Clarke. "The 1929 'Grand Banks' Earthquake, Slump, and Turbidity Current." Geological Society of America Special Paper 229, 1988, pp. 77–92. The modern re-analysis, with multibeam bathymetry showing the actual slide scars on the slope and the deposit thickness on the abyssal plain, and revised timing for two of the cable breaks against the 1952 numbers.
A dev fact for the back pocket
One evening in the first week of September 1992, at a New Jersey diner somewhere between Newark and Murray Hill, Ken Thompson and Rob Pike sat down after dinner with a paper place-mat and worked out the encoding that is now called UTF-8. Thompson wrote the rules on the mat in under an hour; Pike typed them up as an internal Bell Labs memo the following morning; the two of them retrofitted Plan 9 to use the encoding as its exclusive native representation of text over the following week; and Plan 9 shipped as a working UTF-8 operating system in its next distribution in January 1993. The place-mat itself does not appear to survive.
The problem they were solving was that the X/Open Consortium's Universal Character Set working group, in the run-up to what became ISO/IEC 10646-1:1993, needed a byte-oriented external encoding for Unicode that satisfied a specific seven-part list of properties: existing ASCII text had to remain valid without modification; no encoded byte sequence could contain a null byte other than the encoding of U+0000, so C strings would still terminate correctly; the encoding had to be stateless, self-synchronising (from any byte in a stream, a decoder had to be able to find the start of the current or next character within a small fixed number of bytes), and unambiguous (no two Unicode code points could encode to overlapping byte sequences); the encoded length of a character had to be recoverable from its first byte alone; and lexicographic byte comparison of two encoded strings had to preserve the lexicographic order of the underlying code points. An earlier proposal, called FSS-UTF and submitted to X/Open by an IBM committee, satisfied the first four conditions but not the last three and was not self-synchronising under arbitrary substring reads. Thompson's design satisfied all seven simultaneously.
The trick was the specific choice of prefix bits — 0xxxxxxx for a one-byte ASCII character, 110xxxxx 10xxxxxx for two bytes, 1110xxxx 10xxxxxx 10xxxxxx for three, 11110xxx 10xxxxxx 10xxxxxx 10xxxxxx for four — which encoded the length of the character in the high bits of its leading byte and marked every continuation byte with the distinctive 10 prefix. From any byte in a stream a decoder can identify in constant time whether it is a leading byte or a continuation byte; if it is a continuation byte, walking backwards a bounded number of steps reaches the leading byte of the current character; and, because the leading byte of a longer sequence is numerically larger than any single-byte code point and the continuation bytes preserve the ordering of the payload bits, lexicographic byte comparison of two UTF-8 strings gives the same result as lexicographic code-point comparison of the strings they encode. The design does all of this with no lookup table and no state.
Thompson and Pike submitted the scheme to the X/Open working group as FSS-UTF Revision 2 in early September 1992; it was adopted as the definitive encoding of ISO/IEC 10646-1 in 1993 and re-designated UTF-8 in the second edition of the Unicode Standard in 1996. Every subsequent transport of Unicode over a byte-oriented substrate — HTML, JSON, HTTP headers, DNS internationalised domain names, essentially the whole modern web — uses the encoding as it was on the place-mat that September evening, unchanged in the parts that matter.
Primary sources:
- Pike, Rob. "UTF-8 history." Post to the ietf-charsets and ietf-mailing-list, 30 April 2003. Pike's own account, written eleven years after the fact, describing the New Jersey diner, the place-mat, Thompson's derivation, and the week of Plan 9 retrofit that followed. Archived widely; reproduced in full on Pike's personal page at cat-v.org/~rob/.
- Yergeau, F. UTF-8, a transformation format of ISO 10646. RFC 3629, IETF, November 2003. The current normative specification of the encoding. The historical note in Section 1 credits Thompson and Pike, and the introduction lists the seven design properties in essentially their original wording.
- Pike, Rob, and Ken Thompson. "Hello World, or Καλημέρα κόσμε, or こんにちは 世界." Proceedings of the Winter 1993 USENIX Conference, San Diego, January 1993, pp. 43–50. The first published description of Plan 9's UTF-8 implementation, four months after the diner.
Today's goal
Try to say "I was wrong about that" out loud to another human being once today, about something you were actually wrong about — a technical opinion held for a decade that a colleague reversed you on six months ago and you never went back to acknowledge; a person you misread for two years; a tool you dismissed in 2011 that turns out to be excellent; the phrase "I would never" attached to something you now do routinely. The point is not the confession, which is small. The point is the mechanical loosening of the joint. If the sentence can leave your mouth once in an ordinary context, it can leave your mouth in a code review, and if it can leave your mouth in a code review you have escaped malarkey — the ninety-seven-year-old, TAD Dorgan, first-printed-1929 kind — for today.
Today's toy is the mumpsimus ledger — a Victorian correction-book of common wrong beliefs. Each entry states the belief the world still holds and, opposite, the correction the record has already established. friend may receive the correction (a small black stamp lands, the entry updates) or preserve the mumpsimus (a red stamp, the entry stands corrected in the record but the ledger notes friend's continued adherence). The count of preserved mumpsimi is on the spine. It saves. Lives in the corner.
Go get it, friend.
— C