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April 10, 2026
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"The Galápagos Islands, to give one famous example, remained uninhabited by humans until the nine-teenth century, thus preserving a unique menagerie, including their giant tortoises, which, like ancient diporotodons, show no fear of humans."
"... as the travels over the , the rises due to thermal expansion. The Galápagos thermal swell is predicted to be only 400 high (Epp, 1984). The sea floor to the west of is about 3200 m deep, so 2800 m of lava needs to pile up on the swell for an island to form. In reality, much more is required, because as erupts from an oceanic volcano, the extra weight causes the to sag into the , forming a deep root."
"The Galápagos Islands arose as a series of violent volcanic eruptions from a convulsing deep ocean floor on the northeastern section of the . Slowly the islands grew, seething and fuming rising in fiery violence above the surface of the central eastern Pacific in awe-inspiring desolation. In this astonishing isolation they came to harbor living organisms found nowhere else on Earth. Though the islands appear to have no close geologic affinities with the mainland of North and South America, their native derive in the main from the American ."
"... These islands are of particular interest in the , because their study played an important part in inspiring and clarifying Charles Darwin's views upon . The islands are separated from the by a 500-mile expanse of sea of over 1000 s in depth, and through this deep channel there flows a which frequently deposits on their shores , s, s, and other South American products."
"The Galapagos Islands are a global hotspot of environmental change. However, despite their potentially major repercussions, little is known about current and expected changes in regional terrestrial climate variables and s (SST). Here, by analysing existing meteorological observations and secondary datasets, we find that the Islands have warmed by about 0.6 °C since the early 1980s, while at the same time becoming drier. In fact, the onset of the wet season is currently delayed 20 days. This drying trend may reverse, however, given that future climate projections for the region suggest mean annual precipitation may increase between 20 and 70%. This would also be accompanied by more extreme wet and hot conditions. Further, we find that regional SST has increased by 1.2 °C over the last two decades. These changes will, in turn, translate into deterioration of s and , proliferation of , and damages to human water, food, and infrastructure systems. Future projections, however, may be overestimated due to the poor capacity of s to capture Eastern-Pacific dynamics. Our findings emphasize the need to design resilient climate adaptation policies that will remain robust in the face of a wide range of uncertain and changing climatic futures."
"The peculiar character of the Vegetation on the Galapagos Islands was brought to scientific attention in 1847 by Sir . His flora of the archipelago, based chiefly upon the collections of Charles Darwin, showed clearly that these islands, although small in extent, volcanic in character, and only five hundred to six hundred miles from Ecuador, possess a vegetation striking in individuality and very unlike that of the adjacent mainland. Darwin, who visited the Galapagos on the memorable voyage of the " ," landed on four of the islands (, , , and ). He was able to spend only a few days upon each, and naturally much of his attention was devoted to the general topography, the geology, and especially the peculiar fauna; moreover the season was one of drought; yet he was able to collect 201 different plants. These, supplemented by smaller collections (chiefly those of & , , and ), enabled Hooker to include in his enumeration 239 species, of which no less than 107 were described as new to science, thus indicating an extraordinary endemic element of nearly forty-five per cent of the whole flora of the islands, a proportion which became still more remarkable when the imperfectly represented s, and certain s, believed to be artificially introduced s, were omitted from consideration."
"This archipelago consists of ten principal islands, of which five exceed the others in size. They are situated under the , and between five and six hundred miles westward of the coast of . They are all formed of volcanic rocks; a few fragments of curiously glazed and altered by the heat, can hardly be considered as an exception. Some of the craters, surmounting the larger islands, are of immense size, and they rise to a height of between three and four thousand feet. Their flanks are studded by innumerable smaller orifices. I scarcely hesitate to affirm, that there must be in the whole archipelago at least two thousand craters. These consist either of or e, or of finely-stratified, -like . Most of the latter are beautifully symmetrical; they owe their origin to eruptions of volcanic mud without any lava: it is a remarkable circumstance that every one of the twenty-eight tuff-craters which were examined, had their southern sides either much lower than the other sides, or quite broken down and removed. As all these craters apparently have been formed when standing in the sea, and as the waves from the trade wind and the swell from the open Pacific here unite their forces on the southern coasts of all the islands, this singular uniformity in the broken state of the craters, composed of the soft and yielding tuff, is easily explained. Considering that these islands are placed directly under the equator, the climate is far from being excessively hot; this seems chiefly caused by the singularly low temperature of the surrounding water, brought here by the great southern Polar current. Excepting during one short season, very little rain falls, and even then it is irregular; but the clouds generally hang low. Hence, whilst the lower parts of the islands are very sterile, the upper parts, at a height of a thousand feet and upwards, possess a damp climate and a tolerably luxuriant vegetation. This is especially the case on the windward sides of the islands, which first receive and condense the moisture from the atmosphere."
"The Galapagos Islands are well known for their natural beauty and unique wildlife (60% of all organisms are endemic). As on most oceanic islands the native animals show little or no fear of man. These features make the archipelago very attractive for and since 1970 many people have come to see this ‘last paradise’. Initially the flow of visitors caused few problems. Since 1979, however, the pressure on the fragile s has increased rapidly and there is great danger that the archipelago will become another ‘lost paradise’."
"The Galapagos Islands are one of the most productive s in the world. The convergence of four ocean currents and the isolation of these islands create a variety of ecosystems that host unique biodiversity. Many of the endemic species are particularly vulnerable to disturbances in their environment, as most of them are unable to migrate or adapt in response to changing climatic conditions. Due to , there is an increase in extreme weather patterns ( and events) and climate variability. These affect the productivity of marine and terrestrial ecosystems on the Galapagos Islands and ultimately disrupt natural processes and ecosystem dynamics. https://doi.org/10.1016/j.ecochg.2021.100026"
"For ever gaze they at the sea and sky, For ever hear the thunder of the main, For ever watch the ages die away; And ever round them rings the phantom cry Of some lost race that died in human pain, Looking toward heaven, yet seeing no more than they."
"The statues remained quiescent, the natives did not."
"Polynesian Easter Island was as isolated in the Pacific Ocean as the Earth is today in space. When the Easter Islanders got into difficulties, there was nowhere to which they could flee, nor to which they could turn for help; nor shall we modern Earthlings have recourse elsewhere if our troubles increase."
"A Dugong’s and a Porpoise’s skull were produced for barter. The natives evidently treasure skulls of all sorts. Human skulls are likewise kept stuck up in the thatch of the houses."
"There are several Temples in Wild Island; they have already been partially described. One such had as door-posts a male and female figure roughly carved in wood, but elaborately ornamented with incised patterns and colour. Between the legs of the female figure was represented a fish. There are in the same figure black patches with white spots, which appear to mark out the breasts."
Young though he was, his radiant energy produced such an impression of absolute reliability that Hedgewar made him the first sarkaryavah, or general secretary, of the RSS.
- Gopal Mukund Huddar
Largely because of the influence of communists in London, Huddar's conversion into an enthusiastic supporter of the fight against fascism was quick and smooth. The ease with which he crossed from one worldview to another betrays the fact that he had not properly understood the world he had grown in.
Huddar would have been 101 now had he been alive. But then centenaries are not celebrated only to register how old so and so would have been and when. They are usually celebrated to explore how much poorer our lives are without them. Maharashtrian public life is poorer without him. It is poorer for not having made the effort to recall an extraordinary life.
I regret I was not there to listen to Balaji Huddar's speech [...] No matter how many times you listen to him, his speeches are so delightful that you feel like listening to them again and again.
By the time he came out of Franco's prison, Huddar had relinquished many of his old ideas. He displayed a worldview completely different from that of the RSS, even though he continued to remain deferential to Hedgewar and maintained a personal relationship with him.