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Friday, August 7, 2026

Ortega’s Nicaragua is Another Failed Socialist Authoritarian State Oppressing Its Citizens: His Vow of No More Elections Indicates Full-Blown Totalitarianism


     Daniel Ortega, the Reagan-era communist president of Nicaragua, was voted out and got elected again 16 years later, and now continues to rule. The former guerrilla leader was first elected to power in 1984 and was voted out in 1990. He returned in 2007 after losing three presidential elections in between. He served in the government during part of his time between terms. He won the 2006 election with 38% of the vote and has been in power ever since. That gives him about 26 total years in power. He is the longest-serving leader in the Americas. He abolished term limits when he was reelected. In his second term, he has become more and more authoritarian.




      According to Wikipedia:

According to Tim Rogers, writing in The Atlantic, during his second term as president, Ortega took "full control of all four branches of government, state institutions, the military, and police", and in the process dismantled "Nicaragua's institutional democracy". Frances Robles wrote that Ortega took control of "every aspect of government ... the National Assembly, the Supreme Court, the armed forces, the judiciary, the police and the prosecutor's office". In its 2019 World Report, Human Rights Watch wrote that Ortega "aggressively dismantled all institutional checks on presidential power". Many journalists and governments criticize Ortega and label him a dictator.”

     He had been a revolutionary since his teens in the 1960s and was imprisoned for criminal activities, including armed bank robbery and later guerrilla warfare. During the 2008 financial crisis, he declared capitalism a failure. During his last election in 2021, he jailed his opponents. Most recently, he declared that there would be no more elections in the country. He is basically a full-blown dictator. He has become allies with Iran, Colombia’s FARC militants, and other leftist revolutionary groups. He has praised leaders such as Libya’s Gaddafi, Syria’s Assad, Venezuela’s Maduro, and Bernie Sanders, who visited him in 1985. Many protestors have been killed in Nicaragua. The UN called killings during a 2018 crackdown crimes against humanity.   

     Several prominent Nicaraguan opposition figures were exiled in 2023. According to an LA Times article:

Nicaraguans “live in a state of terror,” said Dora María Tellez, a prominent Ortega critic who was imprisoned for nearly two years before she was stripped of her nationality and forced into exile in 2023. Ortega and his wife, Rosario Murillo, whom Ortega named co-president last year, have such a strong grip on power, Tellez said, “that true democratic transition will require intense external pressure.”

Many Nicaraguans have long hoped that Washington would help apply that pressure. Some cheered the stunning U.S. capture of Venezuela’s authoritarian leader, Nicolás Maduro, and support the ongoing White House campaign against Cuba’s communist leadership.”




     While Marco Rubio has condemned Ortega’s statements and actions, Nicaragua, the hemisphere’s second-poorest country after Haiti, does not seem high on the list, since it has not produced many migrants to the U.S. like Venezuela and Cuba.

     Ortega has kept up close ties with Iran and China and continues to criticize U.S. policy and interference in Nicaragua’s and other Latin American countries’ affairs. He has built a system of state surveillance that keeps many Nicaraguans from speaking out.

We cannot raise our voices or express our opinions,” said one woman in Nicaragua who spoke by telephone on condition of anonymity because she fears government reprisals, and who said she would welcome a Venezuela-style intervention by the U.S.

We live with constant dread that at any moment they could seize the property we spent a lifetime working to acquire, or throw us in prison, where we might not make it out alive.”

     It is plainly obvious to many, including me, that the country, much like Venezuela, needs some kind of coerced transition to democracy, especially as the current situation is totalitarian and highly oppressive. One might call it communist oppression. Even many of his socialist revolutionaries have abandoned him and his current dictatorship. Most of those are in exile.

     An article in The Hill by Arturos McFields notes:

The Nicaraguan regime has announced the end of elections. It has decided to establish a formal dynasty that embraces North Korea and defies the new Monroe Doctrine.”

The closeness between the Nicaraguan tyranny and North Korea’s regime is not merely a political metaphor; it is rooted in a historical relationship spanning over 50 years. In 1971, guerrilla fighter Plutarco Hernandez participated in a military training course in North Korea. The objective was to support “the liberation of peoples” — that is, to establish a totalitarian Marxist model in the United States’ backyard.”

In April 1984, Gen. Humberto Ortega — President Daniel Ortega’s brother — traveled to Pyongyang to finalize an arms purchase, even as Nicaragua was starving. For years, the dictatorship blamed the U.S. (“the empire”) for its plight. In reality, the problem lay elsewhere: a model of corruption that squandered millions on weaponry and graft while the people suffered in misery.”

President Ortega and his wife, Rosario Murillo, visited North Korea in September 1986. The Marxist dictator met with the patriarch Kim Il Sung, who expressed solidarity and political support to help strengthen the repressive socialist model.”

Ortega was impressed by the North Korean model — the cult of personality, the elimination of free elections, the absence of political parties and opposition and the lack of checks and balances. It would take many years and many deaths before Nicaragua could replicate this totalitarian family-run model.”

     The bottom line is this guy and his regime are bad news and don’t deserve to be in power. Hopefully, that will change, for the benefit of the oppressed people. One might ask why those in the West who promote an oppressor/oppressed postcolonial narrative don’t speak against such obvious oppression and instead focus on a democracy like Israel. It’s likely because they share his socialist/communist ideology.

     McFields concludes:

The very same regime that has imprisoned bishops and pastors also benefits from a free trade agreement with the U.S. and holds membership in the International Monetary Fund, the World Bank and the Inter-American Development Bank. “

Nicaragua represents a metastatic cancer which, if ignored, could spread to other countries in the Americas, weakening U.S. influence and empowering China and North Korea. The message must be clear: Abolishing elections and crowning oneself king will not be tolerated. It must bring with it serious consequences.”

With dictators like Ortega in Nicaragua — as with Nicolas Maduro in Venezuela — traditional methods never work. A proportional resolve is needed to respond to them, and even an Absolute Resolve should be considered. Hemispheric security is at stake.”


 

References:

 

As Ortega vows to abolish elections, Nicaraguans living 'in a state of terror' hope for US pressure. Kate Linthicum and Ismael López. LA Times. July 26, 2026. As Ortega vows to abolish elections, Nicaraguans living 'in a state of terror' hope for US pressure

Opinion: Nicaragua’s dictatorship defies the Donroe Doctrine. Opinion by Arturo McFields. The Hill. July 29. 2026. Opinion: Nicaragua’s dictatorship defies the Donroe Doctrine

Daniel Ortega. Wikipedia. Daniel Ortega - Wikipedia

Universal Prosperity by 2100: Is it Possible and How Can it Happen? McKinsey Podcast Explores It


     I am a subscriber to McKinsey’s free Weekend Read newsletter, and recently they featured a podcast summary and transcript by members who are the authors of a new book: ‘A Century of Plenty: A Story of Progress for Generations to Come.’ The authors are Sven Smit, Chris Bradley, Nick Leung, and Marc Canal, and each spoke in the podcast. I will summarize and review below.

     They note that the past century’s sixfold increase in global prosperity is a reason for optimism regarding the future. AI, energy, productivity, and innovation are deemed to be the enablers of future prosperity. They say that growth and inclusion should go hand in hand.

     Smit starts the podcast by inviting listeners to imagine the past and then imagine the future. He suggests imagining a prosperous future where GDP per capita is $80,000 in all the countries of the world. Geology and energy expert Scott Tinker and EQT CEO Toby Rice envision $50K per capita as a minimum standard of living sufficient to uplift the poor. Smit then asks if a highly prosperous, 80K per capita future is possible, if so, and how?

     Next, the subject is beliefs about growth. Bradley notes that, according to surveys, most people are not optimistic about a more prosperous future, despite the fact that we have steadily gotten more prosperous over the past century. He notes:

One belief is that growth isn’t good, that it’s destroying the planet, creating inequality, and causing all these problems. Another is that growth isn’t possible, that we’ve reached our limits, that there isn’t enough to keep growing. But maybe the most personal belief is that growth isn’t for me—that I’m not included in growth.”

     I might add that all the news isn’t good. Here in the U.S., it used to take a lower percentage of our income to buy a house or a car. Another fact is that there are capable, intelligent, and creative people even in wealthy countries who are poor and struggling. It seems reasonable to assume that those people have some reason to be pessimistic. Leftists, often in memes, portray these realities to kind of reinforce pessimism about growth and capitalism.

     Canal notes that the numbers are different in China, where surveys find 70% of people optimistic about the future. Leung suggests that this is the case because China’s growth rate has been higher as a developing economy, and that people have seen what growth can do in terms of modernities and better conditions for people in general. I wonder how much of it had to do with fear of saying something against the Chinese Communist Party, thinking about their social scores and surveillance policies. Maybe none at all, I just wonder.

     Smit notes that memories often accentuate the positive, and what people see as the good old days were not so good. We develop a biased view of history akin to nostalgia. Canal simply notes that over the past century, GDP per capita has increased sixfold.

     The next section explores ‘Measures of Progress.’ Canal, who is an economist, notes that while people may not trust GDP as an accurate indicator, that many of the things we care about improved along with it, including higher life expectancy and a huge drop in extreme poverty. Inequality, however, increased. He says inequality is more complicated and will be discussed later. I would say that those other, more important issues to the poor and vulnerable should be prioritized over addressing inequality, although I think we could easily address it with reasonably higher tax rates on the wealthy and super-wealthy. Smit notes that the growth over the past century was not limited and involved periods of contraction, such as the Great Depression, WWII, the oil crisis in the 70s, the dot-com crash, and the 2008 global financial crisis. Bradley notes the work of Hans Rosling, which is covered in the book. Rosling talked about getting to the fourth level of human development as a good life, roughly $32 a day.

     The next section explores what’s directly ahead and how things may be changing. Smit says that in the past, we benefited from globalization, favorable demographics, cheap money, abundant resources, and a growing economy, but things seem to be changing now.

Today, globalization is changing. Technology is no longer just digital. It’s about AI. AI could be incredibly beneficial, but it also introduces new risks. Demographics are no longer providing the same tailwind. We have questions about whether we’ll have enough energy to power AI and whether we can do it cleanly. Where is the cheap money now?

     Bradley cites economist Noah Smith, who suggested people during those massive growth periods of the past century also didn’t see themselves as part of that massive growth and betterment. He notes:

One of our central arguments is that we’ve made enormous progress, but according to the measures we use at MGI, we’re only about halfway toward empowering the world. Our message is: Don’t get off the train halfway through the tunnel. Can we finish the journey?

     Smit notes:

Progress came from a system with many interconnected parts. You could think of it as a machine with eight cylinders. We had more workers. Female labor force participation increased, allowing society to accomplish more. Workers had better tools—what economists call capital. We became smarter as a knowledge economy, developing new manufacturing techniques and new ideas. People increasingly lived in cities, which foster collaboration and productivity.”

     They note that there was a glut of working-age people, but that is changing now as people retire and live longer. Canal notes that we are moving from a demographic dividend toward demographic drag. Smit emphasizes the importance of energy:

I like the second law of thermodynamics, which says that order cannot exist without energy. In a sense, our economy is a form of order. Good food is organized matter. Good cars are organized molecules assembled into something useful. All of this progress came from having more energy while also becoming much more energy efficient.”

     Next, they consider whether growth can be good for the climate. Canal mentions the decoupling that has occurred, which shows that it is possible to improve living standards while also decreasing emissions. Smit notes that it costs money to reduce emissions, which suggests that growth empowers emissions reduction. He notes:

Interestingly, the additional carbon emissions generated by growth are smaller than the additional financial resources that growth provides to solve the problem.”

     He cites success in reversing pollution locally and regionally. In those cases, prosperity enabled environmental protection. It can enable carbon emissions reductions as well. Bradley cites plastic pollution and how much of it is coming from developing countries with inadequate waste collection systems. He notes:

Many environmental problems—litter, deforestation, pollution—actually improve with development rather than worsen. In that sense, more growth, not less, can help solve those problems.”

     Next, they return to inequality, seeing as how economic growth is distributed. Canal notes:

If we look at the world in aggregate as though it were a single country, what’s interesting is that inequality has declined since the 1980s. We first had the Great Divergence, when some countries pulled ahead while others lagged. But over the past 50 to 60 years, inequality has generally been falling. If you treat every human being equally, regardless of national borders, global inequality has been decreasing, and I think that’s good news to begin with.”

     Below, he explains why and how growth is simply better for reducing inequality than non-growth:

There’s a simple piece of arithmetic here. If inequality is to decrease in a stagnant or shrinking economy, someone has to get less for someone else to get more. That’s a much more conflict-ridden world. If you try to reduce inequality without growth, it’s really hard. But when the economy is growing and the pie is getting bigger, it’s possible to reduce inequality while everyone becomes better off. I think that’s simply a much better world to live in.”

     The next section explores affordability and economic empowerment. Smit notes that the affordability of essentials such as energy, education, and housing has become more challenging. He says greater productivity will solve those affordability challenges. At the same time, those “products: need to be produced at a lower cost to buyers. He says there are market failures that need to be acknowledged and addressed, and they can be. Leung explains that purchasing power parity, a measure based on a unit of goods combined with their empowerment calculation, shows that essentials have a disproportionate impact on the poor. They calculated an empowerment line, which is like a poverty line but different, for many countries in dollars per day required for economic empowerment.  

Smit: Our definition of empowerment is different. It means having basic food, shelter, education, healthcare, and a small amount of discretionary income.”

     They note that approximately 4.8 billion people are below that empowerment line and the biggest issue in addressing that is affordability. Bradley points out that it doesn’t really make sense to count on a global poverty number since poverty levels vary considerably by country. That is why an empowerment level is a better indicator. He says it is growth that will bring everyone up to the empowerment line.

     The next section is about trade. Leung notes that the expansion of global trade has been a major part of economic growth. He explains one way they analyzed trade:

As you’d expect, one end of the spectrum includes the United States, the Five Eyes countries [Australia, Canada, New Zealand, the United Kingdom, and the United States], and much of Europe. At the other end are countries such as Russia, China, and Iran, which vote very differently. What we’ve observed over the last several years is that countries are increasingly trading with partners that are geopolitically closer to them. That’s a proxy for what people describe as the fragmentation of the world. There’s been a lot of discussion, particularly in the United States, about decoupling. Our view is that throughout the last century, new forms of collaboration have continually emerged, especially after the Second World War. We haven’t yet figured out the right model of collaboration for today’s geopolitical environment, but we’re confident it can be done. Even if you look at the sheer scale of trade today, intra-Asia trade alone is worth more than total global trade was 25 years ago. The opportunities for productive collaboration remain enormous.”

     Bradley notes that trade can remain robust, even in a multipolar world. Trade is often beneficial in uniting countries, and even countries that have disagreements may still have robust trade. He cautions that strategic technologies such as semiconductors and AI may be subjected to restricted trade, but that is generally not true of basic goods.

     Next, they explore the possibilities of a 2100 economy. They first look at numbers. Population estimates for 2100 vary from a loss down to 8 billion to a rise to as much as 12 billion. According to their calculations, to get all 12 billion people to the level of Switzerland’s GDP per capita would require a growth rate similar to the six-fold growth rate we experienced in the past 100 years. However, the economy would need to grow by 8.5 times. That is much higher than the 2100 estimates by the IMF, the World Bank, and others, which suggest the economy will grow by 3 times.

     In terms of energy, “it’s about expanding total energy availability” as we have been doing. Renewable energy has been growing, but so has fossil energy and all energy. Renewables are just now getting close to matching energy growth. Thus, they are getting close to a point where they actually can replace some fossil fuels. Up to this point, they have not really replaced any fossil fuel energy in total numbers.  

Smit: So imagine an economy that’s 8.5 times larger by 2100, with GDP per capita six times higher and everyone enjoying at least the living standards of today’s Switzerland.”

Bradley: Eventually humanity will reach some limit to growth. My view is simply that we should aim to reach that limit only after everyone enjoys a Swiss standard of living and has the opportunity to live a fully empowered life.”

     Leung says that primary energy would have to increase by 2 to 3 times, but electrified energy would need to increase by 7 to 13 times as more processes are electrified. Low-carbon energy would need to increase by 20 to 30 times. He also says these growth rates are achievable, and that China’s electrification and renewables growth rates are an example. Bradley quips that China’s current growth rate is two to three times what would be needed globally. Nuclear scale-up is also achievable and comparable to France’s 1970s expansion of nuclear growth.

Canal: To put it in context, the scenario we developed assumes that roughly 40 percent of global energy comes from solar and wind, another 40 percent from nuclear, and the remainder from other sources combined with technologies like carbon capture. That scenario certainly won’t be exactly right, but we wanted concrete numbers so we could estimate the required build-out.”

     That would require a huge nuclear buildout, which makes me a bit skeptical. They suggest that 300 new nuclear reactors per year would be required. Smit notes that technologies could have breakthroughs that change the energy scenarios. Perhaps solar and batteries will have a bigger share. Bradley also notes that much more material and minerals would be required; for instance, five times the current amount of copper used in the world today would be required. He also notes that it is doable since proven reserves, not total resources, exceed that amount today.

Bradley: When we examined every major commodity, we didn’t find a single one where projected demand by 2100 came anywhere close to exhausting available resources, even if future reserve growth were only a fraction of what we’ve seen historically.”

Compounding really matters. When we looked across all the materials, we found that available resources, combined with continued improvements in reserves, comfortably supported the levels of growth we’re discussing.”

     The last subject they discussed is AI and automation. These are already replacing humans in the work environment.

Smit: This is where the 8.5-times-larger economy becomes important. Imagine we automate 80 percent of today’s work while the economy only triples. The remaining 20 percent of work becomes 60 percent of today’s total, leaving perhaps 40 percent of people without enough work—or everyone working substantially fewer hours.”

Now imagine an economy that’s 8.5 times larger. Instead of having too many workers, we might actually need more people, or more robots, to keep up. That’s a very different world.”

The key point is that automation doesn’t follow growth. Automation makes things cheaper, and that affordability creates growth. People are beginning to talk about abundance—not universal basic income, but universal abundance. That may sound overly optimistic. But if there’s ever been a time when an 8.5-times-larger economy seems plausible, it’s during the emergence of advanced AI.”

     Finally, Smit gives a summary and the following Five Shifts to Get to Plenty:

First, people have to believe that this future is possible—not guaranteed, but possible. Instead of focusing only on limits, we need to recognize the possibility of abundance.”

Second, we need to believe that growth is fundamentally a good thing, that it helps create prosperity while also giving us the resources to solve the problems we care about.”

Third, we have to believe there’s enough. Enough food. Enough materials. Enough resources for 12 billion people to enjoy at least the living standards of Switzerland today.”

We also need to change our mindset from “it’s complicated to build” to “it’s great to build.” That includes permitting systems and everything else that currently slows progress. The future only arrives if we build it.”

Finally, we need a new narrative. We call it the “narrative of progress.” It’s built around the possibility of a century of plenty—a story worth telling to future generations.”

If all we’ve achieved is encouraging people to raise their ambitions a little and imagine a future of plenty, then I think we’ve done something worthwhile.”

     This was a great discussion of economic possibilities, and I believe what the data is telling us is encouraging, that it can be done. That should be seen as good news. Thus, we should continue to believe in the power of capitalism and economic growth to provide the goods and services we need and to empower all people in the world to decent living standards.

 

 


References:

 

How do we reach universal prosperity by 2100? McKinsey Global Institute. August 5, 2026. Global prosperity by 2100: pathways to inclusive growth | McKinsey

The Denver-Julesburg (DJ) Basin Regains Competitiveness by Increasing Per-Foot Productivity and Drilling Speeds: NOVI Labs Report


      NOVI Labs reports that the Denver-Julesburg, or DJ Basin, has been rebounding due to decreasing costs via faster drilling and higher production per foot. This analysis comes from highlights from a report only available to subscribers, but it gives some important numbers.

The DJ's share of L48 horizontal oil has receded from a peak of more than 7% in 2018 to ~4.5% today; however, per-foot productivity has rebounded to all-time highs, and a 60%+ jump in drilling speeds since the 2023 lows has structurally shifted the cost curve down, making the basin competitive again L48-wide.”

     Major well operators like Chevron and Occidental, and major independents like EOG, are involved in the Colorado play.      

We estimate there are ~108 MM remaining lateral feet (~11k two-mile locations) in the base case or ~18 years of inventory agnostic of asset quality, with that figure rising to ~159 MM feet (~16k locations) with the higher-uncertainty emerging zones included. On stricter risking (an in-zone PDP neighbor within three miles plus a positive NPV25 at mid-cycle and strip), remaining inventory falls to ~89 MM feet, or ~14.8 years at the 2025 drilling cadence. The average NPV25 breakeven across the remaining inventory is ~$58/bbl (assuming $3.50 HH and ~$30/bbl NGLs, pre-differential).”

At the current cadence within the tier-1 rock alone, that tranche of inventory (~27 MM feet) will exhaust in the late 2030's. This update highlights Chevron, Occidental, SM Energy, Bison IV, EOG, and among the smaller operators, Peoria Resources and PEDEVCO.”




    













References:

 

DJ Basin Report Q3 2026. Brandon Myers. NOVI Labs. Email Summary.

Denver Basin. Wikipedia. Denver Basin - Wikipedia

 

      

Floating Wind Power News: Surprising Positive Habitat Impacts, New Structure Design Lowers Turbine Costs by 40%, and China’s Very Large Floating Wind Platform


   

      Fixed-bottom offshore wind turbines are limited to about 60 meters, or 200-feet water depths, which are closer to shore. However, stronger and more consistent winds are more common further offshore, where water depths are much greater. There, floating wind is the technology that works best.

 

Floating Wind Farm Offshore Portugal Found to Have No Ill Effects on Biodiversity and Some Positive Effects

     A floating wind farm 11 miles offshore Portugal, the WindFloat Atlantic project, was the site of a study of its effects on biodiversity. The study concluded that the wind farm had little to no effect on plankton communities or the wider ecosystem. The site even had some positive effects on species abundance, namely fish, octopus, and sole, apparently by improving the substrate of the sea floor. This attracted species like mussels, barnacles, and kelp. The other species were attracted as predators. Apparently, the vibrations of the sea lines that connect the anchors that keep the turbines in place attract the substrate species, creating a reef-like effect.







 

New Design Structure Found to Cut Floating Wind Costs by 40%

     Researchers at the University of Queensland have cut floating wind turbine costs by 40% with a new floating wind design structure. They used a geometry-based approach and tested the design through deep ocean and extreme weather simulations. Floating wind currently costs two to three times more per kilowatt-hour than fixed-bottom offshore wind. The researchers utilized conventional marine construction materials, which are cheaper, easier to source, and familiar to the existing marine industry. The new design is expected to work in water depths of 200 meters.

     According to Interesting Engineering:

The second key innovation is internal stabilization. Features built into the structure lower its center of gravity. A lower center of gravity makes the platform more resistant to rolling and pitching from ocean waves.”




The practical effect is that the wind tower stays vertical even in strong winds. Most floating platforms allow some degree of tilt, which reduces how efficiently the turbine captures energy. A vertical tower keeps the blades facing directly into the wind.”

We also used internal stabilisation features to lower its centre of gravity to make it more stable,” Zhao said. “These features mean it is possible to keep the wind tower vertical even under strong wind conditions, increasing the efficiency of power generation.”

The design also requires less maintenance and is expected to last longer than existing structures. Simulations confirmed it can survive a one-in-100-year storm event.”

     The engineers say that the design is ready to be scaled up to larger turbines and that they are continuing to refine it with further improvements.

 

China Deploys World’s Largest Single-Unit Operational Floating Offshore Wind Turbine

     China’s Three Gorges Corporation (CGT) recently deployed the Sanxia Linghang, or Three Gorges Pilot, which has been described as the world's largest single-unit operational floating offshore wind turbine, by both capacity and rotor diameter. It is a 16MW turbine with an 830-ft rotor diameter and a blade-tip height of more than 885 feet above the water. It floats on a platform in water 164 ft deep.

     According to BGR:

CTG developed a new mooring system, with the 79,000-square-foot floating platform held in place using nine suction anchors and an automatic ballast system for stability. To transfer the generated power to land, the setup uses a 66-kilovolt dynamic cable that's designed to withstand extreme temperatures, wave movement, saltwater corrosion, and mechanical stress, among other challenges.”




     Floating wind farm design with larger turbines could reduce costs by reducing the number of turbines and associated components required per unit of energy. However, BGR also notes some potential caveats to the new, larger turbine design:

It's important to note, however, that various challenges come with these larger, floating turbines. They are, for example, harder to transport and install, not only because of their size but also because working in deep water is more precarious. Additionally, if one of these turbines fails, a lot of capacity is wiped out in one go. Technical issues with smaller turbines are less likely to disable all of them at once, so electricity can continue be produced.”

 


References:

 

A floating wind farm in Portugal is having a surprising impact on underwater habitats. Sead Fadilpasic. BGR. August 1, 2026. A floating wind farm in Portugal is having a surprising impact on underwater habitats

Researchers cut floating wind costs 40 percent just by using basic geometry. Munis Raza. Interesting Engineering. July 31, 2026. Researchers cut floating wind costs 40 percent just by using basic geometry

China's New Offshore Wind Farm Is A Gamechanger For Clean Energy. Trevor Mogg. BGR. June 4, 2026. China's New Offshore Wind Farm Is A Gamechanger For Clean Energy

Biodiversity at the WindFloat Atlantic, Viana do Castelo, Portugal: Non-Technical Summary. March 2026. Estudo-biodiversidade-WFA-2026.pdf

 

 

Thursday, August 6, 2026

The Sacramento Valley Aquifer System: Irreversible Land Subsidence Via Aquifer Compaction Deformation Due to Overuse and Drought, According to Study


      California and much of the U.S. West have been under a drought for many years. The years 2020-2022 were the worst drought years. During those two years, as new research shows, the Sacramento Valley aquifer system was compacted and deformed due to land subsidence. The study measured ground deformation and groundwater levels during the period 2016-2022. Along with the drought, continued high groundwater withdrawals contributed to the subsidence. When groundwater is extracted, the pressure in the aquifer drops, making land subsidence more likely. While some land subsidence is reversible, or elastic, the study confirms that in this case, the subsidence is irreversible, or inelastic. 

     The Sacramento Valley, along with the San Joaquin Valley to the south make up California’s Central Valley, which is responsible for about 25% of U.S. food production.




     The study concludes that the Sacramento Valley aquifer system’s capacity has been permanently reduced as the land subsidence was accompanied by compaction deformation of the aquifer.

"All available measurements suggest that the accelerated subsidence starting in 2021 primarily results from inelastic compaction due to groundwater extraction," the researchers write in their paper.

"On average, the ground surface does not rebound to its pre-2021 state even as groundwater levels recover with seasonal recharge at the end of 2021, indicative of irreversible deformation."





     The result is a permanent loss of storage capacity in the aquifer. Satellites equipped with navigation systems and radar instruments measured ground deformation down to the millimeter level. These are known as Interferometric synthetic-aperture radar, or InSAR. During the period 2016-2020, the data showed that ground subsidence was elastic and returned to its previous level after sufficient recharge. The subsidence during those years was in the range of about 2 centimeters per year, but during 2020-2022, that increased to as much as 50 centimeters per year, 25 times as much. The paper's significance and abstract are shown below, followed by the acceleration in subsidence, a map of the inSAR and groundwater data stations, and historical groundwater level changes.












     The researchers also noted that the methods they used could be used worldwide to monitor groundwater withdrawal-induced land subsidence.

"By imaging this sharp transition at the regional scale, our analysis demonstrates the potential of space-based monitoring for early detection of groundwater overdraft and the resulting loss of aquifer storage capacity worldwide," write the researchers.

     Science Alert explains:

They estimate that the loss of water storage space per year jumped up to 0.2 cubic kilometers (about 7 billion cubic feet) from 2021, around a five-fold increase compared to the previous years.”

That's the equivalent of around 30 percent of the annual water consumption of Los Angeles being lost in terms of capacity: a shrunken aquifer that's not going to be able to store as much water going forward.”

     Importantly, they note that analyzing the network of 2500 groundwater wells did not yet reveal the aquifer changes that the satellite data did, emphasizing the importance of satellite-based land subsidence measurements.

"Real-time monitoring of surface displacements through satellite geodesy, which provide an integrated measure of internal deformation over the entire sedimentary column, could have enabled early detection of this sharp transition and potentially reduced storage loss through timely remedial actions," write the researchers.

"Developing such capability is especially critical in regions where in situ monitoring is unviable but groundwater resources increasingly vital."

     According to the paper, there may have been a shift in the aquifer, which, like many aquifers, has lots of heterogeneity, from withdrawal mainly from coarse-grained, highly permeable rocks to withdrawal from the finer-grained portions of the aquifer.

“…the groundwater dataset is likely skewed toward pressure variations occurring in the coarser-grained, high-permeability aquifer units and the outer edges of fine-grained formations. The in-phase poroelastic response during this period thus suggests that deformation predominantly occurs within these units. In this context, the abrupt acceleration of subsidence in 2021 may indicate a transition from water being primarily drawn from the coarse-grained layers and the edges of adjacent units to significant extraction from the deeper portions of fine-grained units due to higher vertical head gradients associated with increased extraction and decreased recharge during drought periods.”

     The paper’s conclusions are given below and stress the need for more conservative groundwater management strategies in the future.




References:

 

California's drought has now caused irreversible damage to a crucial aquifer. David Nield. Science Alert. August 4, 2026. California's drought has now caused irreversible damage to a crucial aquifer

Central Valley (California). Wikipedia. Central Valley (California) - Wikipedia

Abrupt transition to irreversible damage in the overdrafted Sacramento Valley aquifer system. Stacy Larochelle, Kristel Chanard, Manon Dalaison, Jérôme Fortin, Romain Jolivet, Laurent Longuevergne, Luce Fleitout, Donald F. Argus, Louis-Marie Gauer, and Jean-Philippe Avouac. PNAS. Vol. 123. No. 31. July 27, 2026. Abrupt transition to irreversible damage in the overdrafted Sacramento Valley aquifer system | PNAS

Senate Bill to Aid Microgrids and DERs, Endorsed by DOE, States, and Electrical Manufacturers, Being Considered


     Electrical reliability is a top-of-mind issue these days as demand continues to increase after years of no growth. A Senate bill was recently introduced called the Supporting Transformative Resilience, Operations, and Next-Generation Grid Innovation Deployment, or STRONG GRID Act, which seeks to make microgrids and distributed energy resources eligible for funding under state energy program grants and establish state-run grid resilience programs to support their deployment. The bill would empower a $200 million DOE pilot demonstration project and unleash $500 million in state grants.

The National Association of State Energy Officials, the GridWise Alliance and manufacturers and distributors of grid equipment have endorsed the bill, saying it could help advance the national conversation around grid modernization. “Microgrids, generally, they’re not new. But they’re new to a lot of policymakers and states,” Peter Ferrell, senior director of government relations at the National Association of Electrical Manufacturers, told Utility Dive.”

     Microgrids can advance distributed energy resources (DERs) in the following ways, according to Utility Dive:




     They note that the money for states could do the following:




     Microgrids essentially can aid power system reliability, which is a need that grows alongside demand growth. Microgrids can help during extreme weather events by working to prevent outages. Some can be islanded, providing off-grid power during outages. They can also be built much faster than adding new generation or transmission. They are one tool among several to make grids more resilient and reliable

As grid operators issue resource adequacy warnings and utilities revise demand forecasts upward at an unprecedented pace, tapping into local resources is an increasingly important way to protect communities from reliability risks,” GridWise Alliance CEO Karen Wayland said in a statement.

 

     


References:          

 

$700M microgrid bill has state energy office, electrical manufacturer support: The bill would make microgrids and distributed energy resources eligible for state energy program grants and establish state-run grid resilience programs. Robert Walton. August 4, 2026. $700M microgrid bill has state energy office, electrical manufacturer support | Utility Dive

 

Wednesday, August 5, 2026

Igneous Intrusions: What They Are, Types, and How They Are Formed: Geology Page Explains


     When I did my undergraduate geology field camp in the Valley and Ridge Province of Central Nevada, I encountered igneous intrusions in the field. Specifically, we encountered dikes and sills in outcrop. Dikes are intrusions that cut across the existing rock layers and are typically near vertical in orientation. Sills are more horizontal and typically occur at rock bed boundaries and do not cut across rock layers. One sill I encountered was black with red streaks. I was looking at it from a distance, and I saw movement but couldn’t figure out what it was until I got closer. When I did, I saw that the movement was lizards that had coloration identical to the rock, black with the same red streaks. Those lizards must have evolved to use those particular sills as camouflage.

     Igneous rocks are formed when magma cools after intruding existing rocks or after it erupts from a volcano. Intrusive igneous bodies, also known as plutons, are those that cool and solidify below the surface. The magma that cools after being forced from a volcano is known as an extrusive igneous body. The graphic below from the Geology Page shows the range of intrusive igneous bodies and processes.




     The types of rock that make up igneous intrusions include granite, diorite, gabbro, and tonalite. They generally cool slowly below the surface and are typically coarse-grained. Some volcanic rocks can cool instantly. This is the case with obsidian, which is so very fine-grained and glassy in appearance. They note that:

“…intrusive bodies preserve critical records of magmatic processes, tectonic settings, crustal evolution, and thermal history (Best & Christiansen, 2001).”

     They are valuable for “interpreting magmatic systems, mapping tectonic environments, reconstructing crustal evolution, identifying mineral deposits, and understanding geothermal and volcanic systems.”

     Igneous intrusions may affect and change the surrounding rock through contact metamorphism. The morphology of igneous intrusions depends on magma viscosity, tectonic stress regime, depth of emplacement, composition & temperature, and the mechanical properties of the host rock.

     Batholiths are the largest igneous intrusive bodies. They are defined by a size of over 100 square kilometers and occur when multiple plutons amalgamate over millions of years. The key characteristics of batholiths are that they have an irregular shape and are composed mainly of granitic to dioritic rocks. They represent continental arc magmatism (subduction zones), display zonation: “mafic at margins → felsic at center,” and form deep in the crust (5–30 km depth).

Batholiths reflect long-lived magmatic arcs associated with orogenies.

     Batholiths usually form through successive pulses of magma. Examples are the Sierra Nevada Batholith in the U.S. and the Andean Coastal Batholith of Peru and Chile.

     Dikes cool faster than other intrusive bodies since they reach the less shallow and cooler parts of the subsurface faster. Due to this, they are often more fine-grained than other types of intrusive bodies. Dikes are what bring magma closer to the surface. They often form parallel or radiating swarms. An example is the Mackenzie Dyke Swarm in Canada, the world’s largest dyke swarm.

     Sills typically form under low differential stress. They are commonly associated with contact metamorphism in overlying rocks. They may feature columnar jointing. Examples of sills are the Karoo Sill Complex in South Africa and the Palatine Sill in Scotland.

     Individual plutons are smaller than batholiths, though they may combine to form batholiths. They may be composed of granite (felsic), gabbro (mafic), or diorite (intermediate). Smaller plutons are known as stocks. They often represent the tips of batholiths exposed at the surface.    

     Laccoliths are mostly horizontal dome-shaped intrusions. They are flat at the base with a convex upper surface. They are derived from viscous, silica-rich magma (e.g., rhyolite) and found in shallow crust. They result from higher magma pressure than occurs when sills are formed. An example is the Henry Mountains Laccoliths in the U.S.

     Lopoliths are mostly horizontal saucer-shaped intrusions that are concave-upward. They are often associated with mafic magmatism and form under extensional tectonics, such as rift systems. An example is the Bushveld Complex in South Africa, the world’s largest layered mafic intrusion.

     Pipes are another type of intrusion, although they become extrusive when the volcanoes they feed erupt. There are two types: volcanic pipes and diatremes. Volcanic pipes range from ultramafic to kimberlite. Kimberlite pipes may contain diamonds. Once, when I was working on oil & gas wells in Eastern Kentucky, a guy showed me an industrial-grade diamond that was reportedly found nearby, and we knew that there were kimberlite pipes associated with the Rome Trough, a failed rift one, active at the end of Cambrian time, associated with the opening of the Iapetus Ocean. I even searched near the area where it was said to be found, but didn’t find anything. Pipes can bring magma from deep below the subsurface. Diatremes are explosive breccia-filled conduits.

     Pegmatites are igneous intrusions that are extremely coarse-grained and are often associated with the formation of large crystals of quartz, feldspars, micas, and rare earth minerals. They form from volatile-rich late-stage magmas. Pegmatites are often the source of mineral mines.

     Xenoliths are big intrusions that transport deeper continental rock and magma toward the surface. The “foreign” rock fragments are transported in the magma and retain some of their character. They can be used to study magmatic geochemistry.

     There are three main ways igneous intrusions alter the surrounding rock: 1) Chilled margins, where rapid cooling leads to margins with finer-grained rock; 2) Metamorphic aureoles, where contact metamorphism forms an aureole around the intrusion, typically above it, and 3) Skarns, which result from fluid–rock reactions and metamorphism that can concentrate valuable minerals. I posted fairly recently about a tungsten prospect associated with garnet skarns in Western Idaho. Thermal gradient and time duration determine the metamorphic grade of aureoles and skarns.

     Igneous intrusions have the following textures: Phaneritic Texture: large, interlocking crystals formed during slow cooling; Porphyritic Texture: large phenocrysts set in a finer groundmass; Graphic Texture: intergrowth of quartz and feldspar in pegmatites, and Zoned Minerals: these reflect changing magmatic conditions during crystallization.     

     Geologists identify and study igneous intrusions with the following techniques: 1) field mapping – noting cross-cutting relationships and intrusive contacts; 2) petrography – microscopic analysis of crystals; 3) geochemical signatures - trace elements and isotopes reveal source magmas and crustal contamination; 4) geochronology - radiometric dating (U-Pb zircon) determines when the magmas were placed; 5) geophysics - gravity and magnetic surveys are used to locate intrusions.

    

 



References:

 

Intrusive Igneous Bodies: Types, Characteristics & Geological Processes: Types of Intrusive Igneous Bodies: A Complete Scientific Guide to Plutons, Dikes, Sills, Laccoliths & More. Geology Page. December 5, 2025. Intrusive Igneous Bodies: Types, Characteristics & Geological Processes | Geology Page

     Daniel Ortega, the Reagan-era communist president of Nicaragua, was voted out and got elected again 16 years later, and now continue...