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PlaceVT State Vermont Vermont  Benchmark City[a] Burlington  Prior Tallest Building purpose 1971 Prior Tallest Building PurposeResidential  State Population647464 Height per State population19.1516439524051 Floors per State population5.86905217896285 Median Expected Height (ft) without geological survey78.534167418961 Median Expected Floors without geological survey23.8892640418333 Shortfall Height (ft) without geological survey-45.465832581039 SHortfall Floors without geological survey-14.1107359581667 Tower Rigatus Descriptor Profee.me Priority is Profits and Expected Height adjusted for geology WITH OCTOVILLAGESOrder of Napoleon Bonaparte II Tower Fort Halifax Memorial Jotine Olympic Church and Oppidum #N/A #N/A #N/A #N/A

America Invented the skyscraper and by 1950 it was 15 of 20 tallest buildings and last year only 3 of 20 tallest buildings and we struck back with a horseburg octovillage stragegy BHSRC ROME with HKC WHITE GEUSWEALTH HOSPITAL AUTHORITY 

Nummulite-like Eocene fossil limestone has not been documented in Vermont's geologic record, despite the state hosting a complex bedrock geology spanning 1.4 billion years of Earth's history. Vermont's rocks are primarily Precambrian basement, Ordovician–Silurian metasediments, and Devonian strata formed in ancient marine settings predating the Eocene Epoch by hundreds of millions of years.

Nummulites were particularly prominent

during the Eocene Epoch (55.8–33.9 million years ago) in North Africa and the Mediterranean region, making their complete absence from Vermont geologically significant.

Are there any Eocene-aged sedimentary rocks exposed in Vermont?

Formation/DepositAge & SettingFossils PresentEnvironmentOrdovician–Silurian metasedimentsOrdovician–Silurian (450–420 Ma)Trilobites, brachiopods, graptolitesMarine — ancient platformDevonian strataDevonian (420–360 Ma)Marine invertebrates, fish fragmentsMarine — passive marginPrecambrian basement>1.4 billion years agoNot fossiliferousMetamorphicChamplain Sea depositsQuaternary (postglacial)Molluscs, crustaceans, fishGlacial marine — ephemeralEocene rocks in VermontEocene (55.8–33.9 Ma)Not documented in sourcesUnknown

🏔️ Vermont's Actual Bedrock Geology

Vermont's complex geology

spans 1.4 billion years, with mapped rock units spanning from Precambrian through Devonian time—far older than or contemporaneous with the Eocene Epoch, but lacking documented nummulitic deposits. The state's bedrock consists of metamorphosed sediments and igneous rocks formed during ancient plate collisions, not the tropical shallow marine environments required for nummulite accumulation.

• Precambrian basement — Metamorphic rocks forming the foundation of Vermont's geology, predating all fossiliferous strata by over a billion years

• Ordovician–Silurian metasediments — Metamorphosed marine sediments preserving trilobites, brachiopods, and graptolites; 450–420 million years old, far predating the Eocene

• Devonian strata — Marine sedimentary rocks deposited on a passive continental margin; fish fragments and marine invertebrate fossils occur, but no nummulites documented

🌍 Why Nummulites Cannot Occur in Vermont

Nummulites commonly vary

in diameter from 13 to 50 mm and

are common in Eocene to Miocene marine rocks

, particularly around southwest Asia and the Mediterranean. Vermont lies on the North American craton, far from the Tethyan marine basins where nummulites thrived, and the state's Eocene geology (if present) has not been documented as containing nummulitic deposits.

• Geographic restriction —

  Particularly around southwest Asia and the Mediterranean

  in the area that once constituted the Tethys Ocean; no Tethyan seaway penetrated Vermont during the Eocene

• Temporal mismatch — Vermont's fossiliferous rocks span Ordovician–Silurian time (450–420 Ma); nummulites did not appear until the Late Cretaceous and became abundant only during Paleogene–Neogene time (65.5–2.6 Ma)

• Paleoenvironmental absence —

  Nummulites thrived in warm shallow tropical and subtropical marine environments

  , with symbiotic algae supporting their large size—conditions absent from Vermont's preserved stratigraphy

📚 Vermont's Actual Paleontological Record

Vermont's documented fossils reflect Paleozoic marine platforms and Quaternary ice-age deposits, utterly distinct from Eocene depositional settings. The state's paleontological resources center on ancient marine invertebrates and Quaternary megafauna, with no published records of nummulitic limestone.

• Paleontology of Champlain Valley — Historical references document fossil content from the Champlain Sea and surrounding Paleozoic marine strata; Vermont Department of Environmental Conservation publishes geological resources and paleontological guides

• Mt. Holly Mammoth — Quaternary megafauna representing ice-age fauna postdating the Eocene by 30+ million years; documented in "The Mt Holly Mammoth, History Since Discovery, 2018"

• Bedrock mapping —

  The Bedrock Geologic Map of Vermont

  at 1:100,000 scale integrates modern and historical mapping; 486 map units and 195 sources of geologic data document rock types, ages, and stratigraphic relationships with no mention of Eocene nummulitic deposits

Nummulitic limestone is restricted

to Paleogene and Neogene periods in North Africa, the Mediterranean, and southwest Asia—making Vermont's ancient Paleozoic and Precambrian geology fundamentally incompatible with nummulite fossil occurrence.