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A place where you can live from the inhibtion of science
Perhaps in a few days once I learn some more about them and go through all the links and stuff, I'll post something a bit more substantial.
Originally posted by sardion2000
When I get my PhD, I want to start a Gaviotas in Canada. As far North as possible,
Originally posted by Relentless
Originally posted by sardion2000
When I get my PhD, I want to start a Gaviotas in Canada. As far North as possible,
Okay, I want in but not where it's cold. Can't you find someplace else to inspire you?
Oh, and how long till you have a PhD? Will you be letting old ladies in then?
Gosh, I really envy this group. I have to start reading up on this. They sound like a ray of hope in the world.
Honestly, I think you are over complicating this issue. It comes across as very rigid, lacking room for creativity and time consuming. I doubt they go into so much detail regarding creating and filling a job at Gavioas do they?
The Bounty Economy is not a complex topic. Essentially it's merely a wide open invitation to ideas for solving problems for a fee, presented to all comers. In a global economy, rife with cut throat competition, such methods for dealing with tough problems are increasingly hard to beat. Especially now that ever improving computer software and performance allows for easy analysis, comparision, and judgement of the value of thousands of ideas per minute. Of course, credibility, accountability, and fairness rule supreme in the process-- illegitimate offers usually ruin forever the chance for the offending entity to successfully field such bounty offers again-- as the bounty economy's memory is forever.
The scientists (Bogota engineers) weren't seeking an alternative lifestyle
so much as applying common sense to use what little materials lay at hand.
[...barren, sparsley settled savannas constitute much of the tropics...]
It is a wonderful thing this community has achieved, and it belongs to them alone. Nothing like that can ever be reproduced in the states, and I do not believe the climate anywhere in Canada would be right for it. How many different kinds of crops are grown up there anyways?
either way, with all the obstacles ahead of yall, I wish you good luck in your efforts Sardion. I would definetly visit any successful sustainable townships you and others may develop in the future, although my advice would be to just join them.
Trust me Colombia is not as scary as the Western news used to make it out to be, and you already know for the most part the town itself is safe.
Kinsale Energy Descent Plan (PDF Warning)
The story of the Kinsale Energy Descent Action Plan is an extraordinary one. A mid-thirties Englishman with a penchant for permaculture and an interest in peak oil moves to rural Ireland, starts teaching at the local further education college, and ends up writing, with his students, a ground-breaking document: the first timetabled strategy for weaning a town off fossil fuels. And what is more, that small Irish town actually adopts the action plan and starts to implement it.
Kinsale is a seaside town of 7000 inhabitants renowned as Ireland’s gourmet food capital, as well as the home of a well-known jazz festival. Kinsale 2021 is the title of the document: Rob Hopkins is the man, who persuaded Kinsale Further Education College to start the first full-time two year course in Europe training in people in Practical Sustainability.
Originally posted by sardion2000
Here is a research program that is similiar to what I plan on doing.
www.bluemountainpeakranch.com...
This project is in Texas.
GEOLOGY AND HYDROGEOLOGY OF THE FAULT-PARTITIONED HICKORY AQUIFER IN NORTHERN MASON COUNTY, CENTRAL TEXAS
The Cambrian-age Hickory Sandstone is a major aquifer in Central Texas. The Hickory Sandstone is a 450 ft (137 m) thick, high porosity, siliciclastic unit that unconformably overlies Precambrian crystalline basement. A system of N- and NE-trending normal and oblique-slip faults structurally partition the Hickory Sandstone aquifer within the study area in northern Mason County. Typically, the Hickory Sandstone is only partially offset across the faults and portions of the saturated interval of the aquifer usually are juxtaposed against each other across the faults. Exposures of shear zones of faults in sandstone horizons exhibit significant grain comminution and porosity reduction; shear zones containing deformed clay interbeds, however, are not exposed.
The observed spatial and temporal variations of water levels in wells in the study area clearly show that faults impede the lateral flow of groundwater and influence both the short- and long-term hydraulic responses of fault-defined regions. The existence of a low conductance fault is indicated by one or more of the following features: 1) an anomalously large hydraulic-head change across the fault, 2) a significant variation of the hydraulic gradient in proximity to and on either side of the fault, and 3) poor or indiscernible hydraulic communication between wells on either side of the fault. In general, the greater the displacement of a fault, the greater is the effect of the fault on the groundwater system. Discernible effects are observed for discrete faults with displacements as small as 50 to 75 ft (15-23 m). Regions with numerous small faults dramatically reduce production rates of wells.
The study area can be subdivided into at least three major hydraulic compartments with boundaries defined by faults with at least 100 ft (30 m) of displacement. Poor hydraulic communication exists between wells in neighboring major hydraulic compartments, such that irrigation pumping in one compartment induces in the neighboring compartment an anomalously small drawdown relative to that expected in a laterally uniform aquifer. The major hydraulic compartments are further subdivided into subcompartments by faults across which there is relatively good hydraulic communication, yet the faults still influence the short-term water-level variations within the subcompartments. Following a long period of sustained pumping, residual drawdowns after a short time of recovery (5-12 days) differ significantly from compartment to compartment. Pumping-induced drawdown and recovery characteristics are similar for wells within the same major hydraulic compartment, but often differ from those of wells in adjacent compartments. These differences reflect, in part, the differences in the areal extent of the compartment and the rate of groundwater flow into and out of the compartment. Annual and longer-term water-level declines differ significantly among the hydraulic compartments, which reflects a limited flow of groundwater from a hydraulic compartment positioned up-gradient into an adjacent down-gradient hydraulic compartment.