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It all started here.

It all started here. With Platform A: the first of thirty-some oil platforms built in the 1960s off the coast of Southern California. To anybody looking seaward from Santa Barbara, the platforms are nearly as much a fixture of the horizon as the Channel Islands beyond. The three closest, Platforms A, B and C, are just several miles out.

On January 28, 1969, Platform A had a blow-out. As much as 100,000 barrels of oil rose to the surface and spread. Had the oil been carried away from shore, the event might have been small news. But instead it gunked up the coast, ruining Santa Barbara’s harbor for a time, and treating the world to the first of many iconic visuals: tar-covered sea birds.

Long story short, Earth Day followed.

Some pictures from the time.

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I’m listening right now to On Point*, where the topic is Pushing E-Health Records. The only case against electronic health records (EHR, aka electronic medical recordsk, or EMR) is risk of compromised privacy. Exposure goes up. The friction involved in grabbing electronic medical records is lower than that involved in grabbing paper ones, especially with the Internet connecting damn near everything.

Here’s the problem with privacy in the Internet Age (which we are now in, with no hope of ever getting out, unless we live the connectionless life): the Net is a big copy machine. It’s amazing how a fact so simple escapes attention until a first-rate metaphorist such as Kevin Kelly comes along to expound on what ought to be obvious:

The internet is a copy machine. At its most foundational level, it copies every action, every character, every thought we make while we ride upon it. In order to send a message from one corner of the internet to another, the protocols of communication demand that the whole message be copied along the way several times. IT companies make a lot of money selling equipment that facilitates this ceaseless copying. Every bit of data ever produced on any computer is copied somewhere. The digital economy is thus run on a river of copies. Unlike the mass-produced reproductions of the machine age, these copies are not just cheap, they are free.

Our digital communication network has been engineered so that copies flow with as little friction as possible. Indeed, copies flow so freely we could think of the internet as a super-distribution system, where once a copy is introduced it will continue to flow through the network forever, much like electricity in a superconductive wire. We see evidence of this in real life. Once anything that can be copied is brought into contact with internet, it will be copied, and those copies never leave. Even a dog knows you can’t erase something once it’s flowed on the internet.

We’re not going to fix that. The copying nature of the Net is a feature, not a bug. We can fight some of it with crypto between trusting parties. But until we find ways to make that easy, the exposure is there. And, as long as it is, we’re going to have people who say risk of exposure overrides other concerns, such as the fact that dozens of thousands of people in the U.S. alone die every year of bad health care record keeping and communications — in other words, of bad data.

Still, if we want good medical care, we need EHR. That much is plain. The question is, How?

The answer will not be an information silo, or a set of silos. We have too many of those already. That’s the problem we have now — both on paper and in electronic formats (as I discovered last year in one of my own medical adventures).

The patient needs to be the point of integration for his or her own data, and the point of origination about what gets done with it. Even if the patient’s primary care physician serves as a trusted originator of medical decisions, the patient needs to anchor the vector of his or her own care, for the simple reason that the patient is the one constant as he or she moves through various medical specialties and systems.

The patient needs to be the platform. Not Google, or Microsoft, or your HMO, or the VA, or some kieretsu involving Big Pharma, Big Software Companies and Big Equipment Makers.

This requires classic VRM: tools of independence and engagement. That is, tools that enable the patient to be independent of any health care provider, yet better able to engage any provider.

In other words, while the answer needs to be systematic, it does not need to be A Big System (which I fear both BigCos and BigGovs whish to provide).

The answer needs to come from geeks who know how to eliminate big problems with simple solutions. For example,

  • Consider how the Internet Protocol solved the problem of multiple networks that didn’t get along.
  • Consider how email protocols such as SMTP, POP3 and IMAP solved the problem of multiple email systems that didn’t get along.
  • Consider how the XMPP protocol solves the problem of multiple instant messaging systems that don’t get along.

We need new ways of organizing our own health care data, and communicating that data selectively to trusted health care providers through open and standard protocols (that may or may not already exist… I don’t know).

I wanted to get those thoughts down because there’s a bunch of stuff going on around health care right now (including two conferences in Boston), detailed to some degree in Health Care Relationship Management, over at the ProjectVRM blog.

* On WBUR, a Boston station I pick up here in Santa Barbara over my Public Radio Tuner.

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Good of Vanity Fair to interview some of the Net’s and the Web’s fathers and sons (alas, no mothers or daughters), in a piece titled How the Web was Won.

On vision:

Leonard Kleinrock: Licklider was a strong, driving visionary, and he set the stage. He foresaw two aspects of what we now have. His early work—he was a psychologist by training—was in what he called man-computer symbiosis. When you put a computer in the hands of a human, the interaction between them becomes much greater than the individual parts. And he also foresaw a great change in the way activity would take place: education, creativity, commerce, just general information access. He foresaw a connected world of information.

The culture was one of: You find a good scientist. Fund him. Leave him alone. Don’t over-manage. Don’t tell him how to do something. You may tell him what you’re interested in: I want artificial intelligence. I want a network. I want time-sharing. Don’t tell him how to do it.

On intellectual property sanity:

Larry Roberts: After we built the Arpanet, lots of people built networks. Everybody was competing. Everyone had their own thing that they wanted to do. So it became very important that the world have one protocol, so they could all talk to each other. And Bob Kahn really pushed that process. And Vint. And it wasn’t licensed. They proved to the world that making something free as a driver would make a huge difference in making it a standard.

Robert Cailliau: We looked for a name for several weeks and couldn’t come up with anything good, and I didn’t want yet another one of these stupid things that doesn’t tell you anything. In the end Tim said, Why don’t we temporarily call it the World Wide Web? It just says what it is.

At one point cern was toying with patenting the World Wide Web. I was talking about that with Tim one day, and he looked at me, and I could see that he wasn’t enthusiastic. He said, Robert, do you want to be rich? I thought, Well, it helps, no? He apparently didn’t care about that. What he cared about was to make sure that the thing would work, that it would just be there for everybody. He convinced me of that, and then I worked for about six months, very hard with the legal service, to make sure that cern put the whole thing in the public domain.

On how markets are conversations after all:

Steve Case: We always believed that people talking to each other was the killer app. And so whether it was instant messaging or chat rooms, which we launched in 1985, or message boards, it was always the community that was front and center. Everything else—commerce and entertainment and financial services—was secondary. We thought community trumped content.

On the dawn of a different democracy:

Wes Boyd: I think the biggest shock for us, and it was from the very beginning, was not: Oh, boy, these big people are paying attention to us. It was that there are no big people; it’s up to all of us. And that’s a very scary thing, you know, when you realize what a vacuum there is in many ways in politics.

On the end of media as usual:

Dave Winer: The press is very susceptible to conventional wisdom. The press buys into certain things being true that really aren’t true. The conventional wisdom was that Apple was dead and there was no new software for Macintosh. Yet I was a software developer making new software for the Macintosh. So I went to bat for Apple.

That was the reason why I got so heavy into blogging—I didn’t want the verdict of the press to be the last word. And I’d argue that the same thing is happening now in politics. Today it’s: Is Reverend Wright really a disaster for the Obama campaign? Well, the press seems to think so, but if we want to get a different story out there we’re going to have to do it ourselves.

It’s far from a Compleat History, but it’s a fun read. Makes me wish The Media (including bloggers) had reported more about What Happened after Gutenberg invented movable type. I don’t think the parallels would be few.

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Props to Joe Andrieu for pointing out the Cult of Done, for which I am constitutionally disqualified, but wish I were not.

Why? Because I: 1) Bite off more than I can eschew, 2) Keep more balls on the floor than anybody I know, and 3) Plan for my epitaph to read “He was almost finished.”

But I am at home right now, mostly getting things done while regretably missing Free Libre Planet, happening right now at Harvard, and for which I am registered. Just too much to catch up on, and I don’t know when Wes Felter is speaking. Hope it’s tomorrow, by which time I hope to have more done.

Ah, I see that Wes’ personal servers is up for an unconference session tomorrow. I’ll be there for that. Yay.

Here at SXSW there are two conferences happening on the same floors: Interactive and Film. Interactive is mostly computing geeks. Film is mostly film geeks.

The main visual difference: tatoos and laptops. In the film crowd there is a high tatoo/laptop ratio. In the interactive crowd, there is a high laptop/tatoo ratio — lthough many laptops have tatoos in the forms of decals, which are left on tables and handed out to attendees by companies or causes with something to promote.

I’m on the Interactive side, but have attended very few sessions here, mostly because we have a bunch of VRM developers here, and are taking advantage of sharing meet/meat space to get stuff done. It’s been very productive, actually.

Anyway, I decided yesterday to visit one of the film sessions: the enthusiastically titled Henry Selick and Robert Rodriguez talk 3D at SXSW! The room was packed. The only laptops I saw were my own and two others in the back row. It felt only a bit less strange than it did seven years ago when I attended my first Digital Hollywood in Los Angeles. Back then computer users and Hollywood were at “war.” Or so the Hollywood folks said. “Piracy” was the big topic. I didn’t raise my flag.

A little different now. Great session too, by the way.

If you want to keep something in orbit around the Earth, you need it to be flying parallel to the surface at speeds exceeding those of bullets. Get high enough above atmospheric drag, and stuff will continue to orbit as long as the moon does.

The moon has been around for 4,530,000,000,000 years, give or take.

Humans have been throwing junk into space, and occassionally blowing orbiting crap into countless smithereens, for about fifty years. As a result, the risk of impact to large objects such as shuttles, observatories and space stations is one-in-a-few hundred.

Or, in the case of the International Space Station, one-in-what? Today the ISS was evacuated, just in case.

#iss tweets.

Since it’s obvious that it’s a bad idea to fill the orbital environment with junk that’s damn near impossible to get rid of, why do we keep doing it?

Because every species operates in its own flawed self interest, I guess.

Love this line, from Dave: I have no idea how these guys got the idea that they could save the news industry by becoming the tech industry.

Dave’s the only guy I know who reliably schools both the journalism and the tech industries, often at the same time. Well done.

So our Verizon FiOS home bill has been about $160/month. We were looking to chop that down a bit when I called Verizon this morning.

To put it as simply as possible, it’s complicated.

What I care about most is keeping the 20/20Mbps down/up Internet service. That’s $69.99/mo.

What I don’t care about is POTS, or Plain Old Telephone Service. So I canceled that. We use cell phones, and we’ll find another way to fax, as rarely as we do that.

That leaves TV.

What we still call TV isn’t what it used to be: channels on a dial. They are digital program sources that are organized by “channels”, but that’s a legacy convenience. A few are available over the air, as DTV signals. Those are…

  • WGBH-DT (still called Channel 2, actually on Channel 19). It also has an SD (standard definition) version. These are called 2-1 and 2-2, or WGBG-DT1 and WGBH-DT2. Affiliated with PBS.
  • WBZ-DT (still called Channel 4, actually on Channel 30). Affiliated with CBS.
  • WCVB-DT (Still called Channel 5, actually on Channel 20). Affliiated with ABC.
  • WHDH-HD (still called Channel 7, actually on Channel 40). Also called 7-1, It has a second channel on 7-2 called This TV. It’s SD. Affiliated with NBC.
  • WFXT-DT (still called 25, actually on Channel 31). Affiliated with Fox.
  • WSBK-DT (still called 38, actually on Channel 39). Independent. Owned by CBS.
  • WGBX-DT (still called 44, actually on Channel 43). Four SD channels, labeled 44-1 through 44-2. Called WGBX, World, Create and Kids. Affiliated with PBS.
  • WYDN-DT (still called 48, actually on Channel 47) with a directional signal). The picture is SD. Affiliated with Daystar. Evangelical Christian.
  • WLVI-DT (still called 56, actually on Channel 42 with a directional signal). Affiliated with CW.
  • WMFP-DT (still called 62, actually on Channel 18 with a directional signal). Labeled 61-1 and 62-2. The second is currently dark. Affiliated with Gems TV. Home shopping.
  • WBPX (still called 68, actually on Channel 32, with a directional signal). It’s four channels in one, all SD: WBPX Digital Television, Qubo, Eye on Life and Worship. Identified on the tuner as 68-1, 2, 3 and 4. Affiliated with ION Television.

For what it’s worth, I get all those on my laptop with a little adapter. Meaning that I don’t need cable for them. They’re free. They cost $0.00.

Okay, so Verizon offers two channel lineups in our region: Essentials for $47.99/mo. and Extreme HD for… I can’t find it now. $57.99/mo, I think. Essentials has the about same minimun channel line-up I get for free over the air. Extreme HD has what you want if you watch in HD: all the main cable and sports non-premium channels. Add DVR rental (for which one has no choice) for $12.99 and I’m at $140 or so, if I want the Extreme HD.

TV now is an HD deal. If you want TV, you want HD, because that’s the new screen you’ve got, even if you’re watching on a laptop.

The problem is, HDTV costs you. Unless you want the minimal legacy lineup of local over the air channels.

Anyway, here’s what I want: a la carte. Across the board. I’m glad to do Pay Per View for everything.

And right now I’m thinking hard about cancelling the Extreme HD I just ordered. We like the sports and the movies, but we can go to a bar for the former and get the rest from Netflix or something.

Meanwhile, kudos to Verizon for providing fiber, and the 20/20 connection. Here’s another message: I’d gladly pay more for even more speed. Especially upstream.

[Later…] Now I’m looking at the Verizon Massachusetts channel lineup and it seems like the only thing extra I get with Extreme HD is some sports channels. Is that right? Sports-wise, all I care about are NESN, ESPN, TNT and other Usual Suspects.

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Says here that sex came along at least 365 billion million years ago.

Magma roots

capitol reef

The problem with “grass roots” as a metaphor is that it reduces its contributors to the miniscopic. Not microscopic, because then you couldn’t see them without a microscope. But miniscopic, meaning they’re small. You have to get down on all fours to eyeball them and say hi.

So I’ve been thinking about alternative meaphors where large movements are involved. For that you have to go deeper. Not into the dirt, because that has connotations of filfth and death. Rock roots is okay, in the sense that serious rock for the most part is solid, or what geologists call “competent”. You can build on it, and with it. The largest slabs of it are “tectonic”.

But maybe we can go deeper than that, below the Earth’s crust. How about “magma roots”? That occurred to me while reading Ron Schott‘s post, Building a Google Earth Geology Layer. Ron is a hard rock geologist who has been a good source of wisdom (and occasional correction) toward my own geology obsessions. What Ron proposes (in both his posts title and its detail) is a great idea — for Google, for the geology field, and for the rest of us.

Ron’s goals are modest in manner and ambitious in scale:

What I’d like to do here, with the help of the geoblogosphere (via the comments to this post, initially), is to set out some goals, examples, and use cases that could guide the development of a Google Earth geology layer. If there’s interest in building on this idea, I’d be happy to set up communications tools, create KML tutorials, or do anything else to facilitate a coordinated effort to develop such a layer. Hopefully, by leveraging the knowledge and efforts of the geoblogospheric community, along with excellent new resources for developing KML, we can make a real start toward building a useful geology resource.

For now, what I’d like to do is to begin to collect best practices/examples of good uses of KML in illustrating geology in Google Earth. I’ll start by pointing out the USGS Earthquake Hazards Program’s collection of Google Earth KML files and another collection of geologic KML resources at San Diego State University. These should give you some idea of the sorts of things that will be possible. Also helpful would be use cases – how would you like to use a geology layer in Google Earth? Suggestions here will offer us guidance as to what the most important elements of a Google Earth geology layer should be.

I’m not a geologist, but I want to do everything I can to help raise this barn. Or, to keep from mixing metaphors, uncork this volcano.

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