A non-moron would note that there's no sign of elevated temperatures in the oceans immediately over those volcanoes. Hence, they're not melting any ice. Their heat output is so comparatively tiny, it doesn't even register in the ocean environment.
Let's run some numbers.
Latent heat of melting for water = 334 kJ/Kg
Mass of ice melting = 219 E12 kg/year
That makes 73 E15 kJ/year energy being used to melt ice.
The volcanic output of the whole planet was estimated at 5E13 kJ/year for 2001.
Satellite tots up volcanic heat : Nature News
So, the Antarctic ice melt alone would require 1400 times the global volcanic heat output of a "quiet" volcanic year.
Now, a large volcano will release much more heat, but it would be impossible to miss such eruptions. According to SSDD's theory, there would have to be dozens of Mt St. Helens scale eruptions going off every year under the ice, suddenly starting just a few decades ago, but we've never been able to detect them. Being that's a nonsensical theory, everyone laughs at it.
Poor hairball....is it that you are to stupid to actually look beyond the information given to you by your high priests?...or is it more of a theological issue with you...do you think it is unseemly, or improper for a lay person to question what one of the high priests tells you? Or is it just that much easier to be a dupe?
Cleary you didn't read any of the information I provided regarding the volcanic activity under the western antarctic. Instead, you go back to an old article published before science even started looking in any real way for volcanic activity under antarctica. Your article is from 2004, scientists weren't even clued into volcanic activity under the WAIS till 2007...What a dupe..
Here, from the first source I provided:
Clip: Subglacial meltwater movement under the Thwaites Glacier was mapped with radar-based methods. The result is that meltwater production is very unevenly distributed. This can be used to calculate
the geothermal heat flux under the glacier, which reaches values up to 200 milliwatts per square metre while averaging near 100 over the whole area. In comparison, the average value for all continents on Earth is just near 65 milliwatts per square metre.
Don Blankenship, scientists of the University of Texas and one of the author of a recently published study, described the Thwaites Glacier as follows: The glacier “sits on something more like a multi-burner stovetop with burners putting out heat at different levels at different locations. …
Here, from the second source...the national science foundation...you guys reference them all the time...
Clip: Tracing a chemical signature of helium in seawater, an international team of scientists funded by the National Science Foundation (NSF) and the United Kingdom's (U.K.) Natural Environment Research Council (NERC) has
discovered a previously unknown volcanic hotspot beneath the massive West Antarctic Ice Sheet (WAIS).
The researchers first noted the volcanic activity in 2007 and verified its existence again in 2014.
"Our finding of a substantial heat source beneath a major WAIS glacier highlights the need to understand subglacial volcanism, its interaction with the marine margins and its potential role in the future stability of the WAIS,” they write in the
Nature Communications article.
They also note that volcanic activity could be increasing the rate of collapse of the Thwaites Glacier, which is adjacent to the Pine Island Glacier.
And from the third source...also from Nature...but publshed in 2018 rather than 2004.....
Clip: Here we show geochemical evidence of a volcanic heat source upstream of the fast-melting Pine Island Ice Shelf, documented by seawater helium isotope ratios at the front of the Ice Shelf cavity. The localization of mantle helium to glacial meltwater reveals that volcanic heat induces melt beneath the grounded glacier and feeds the subglacial hydrological network crossing the grounding line. The observed transport of mantle helium out of the Ice Shelf cavity indicates that volcanic heat is supplied to the grounded glacier at a rate of ~ 2500 ± 1700 MW, which is ca. half as large as the active Grimsvötn volcano on Iceland. Our finding of a substantial volcanic heat source beneath a major WAIS glacier highlights the need to understand subglacial volcanism, its hydrologic interaction with the marine margins, and its potential role in the future stability of the WAIS.
Plenty of modern, credible evidence of volcanic activity under the glacier and in your irrational state of denial, you refer to information published several years before volcanic activity under antarctica was any more than a tiny blip on the radar.