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14 results for "Yucatan karst"
D_4_09 — Cenotes: Maya Sacred Wells, Karst Hydrology, and Underworld Cosmology
Cenotes (from Yucatec Maya dz'onot or ts'onot) are natural sinkholes formed by the dissolution and collapse of limestone bedrock in the Yucatan Peninsula, exposing the vast underground freshwater aquifer beneath. Over 6,
O_5_09 — Karst Topography: Towers, Sinkholes, and Dissolved Landscapes
Karst topography is a distinctive landscape formed by the chemical dissolution of soluble bedrock — primarily limestone (CaCO₃), but also dolomite, gypsum, and evaporites — by naturally acidic water (CO₂-enriched rainwat
O_3_12 — Cenote and Sinkhole Ecology — Surface-Groundwater Connections
Cenotes (from the Maya ts'onot) and sinkholes — natural depressions or holes formed by the dissolution of soluble bedrock (limestone, dolostone, gypsum) in karst landscapes — are far more than geological curiosities. The
O_3_15 — Blue Holes: Submerged Sinkholes & Marine Geology
Blue holes are submerged sinkholes or vertical cave systems formed in carbonate rock (limestone, dolomite) during periods of lower sea level and subsequently flooded by rising oceans. Named for the deep blue color that c
O_3_08 — Subterranean Rivers and Underground Water Systems
Subterranean rivers and underground water systems represent one of Earth's most extensive yet least visible hydrological features — approximately 30% of the world's freshwater (excluding ice caps) exists as groundwater,
W_4_01 — Maya Epigraphy, Astronomy, and Calendar Science
The Maya civilization developed one of the most sophisticated writing systems in the pre-Columbian Americas — a mixed logographic-syllabic script that recorded history, astronomy, mythology, and ritual on stone monuments
E_4_27 — Chicxulub Impact and the K-Pg Mass Extinction
The Chicxulub impact was a catastrophic asteroid strike that occurred approximately 66.043 ± 0.011 million years ago at what is now the Yucatan Peninsula, Mexico, marking the boundary between the Cretaceous and Paleogene
E_1_06 — Chicxulub Impact and the K-Pg Boundary
Approximately 66 million years ago, at the boundary between the Cretaceous and Paleogene periods (K-Pg boundary, formerly K-T boundary), a ~10 km diameter asteroid struck what is now the Yucatán Peninsula of Mexico, crea
ZB_4_10 — Cave Ecology: Life in Perpetual Darkness
Cave ecology (speleobiology) investigates life in subterranean environments — caves, groundwater aquifers, lava tubes, and interstitial spaces — habitats characterized by permanent darkness, near-constant temperature, hi
ZB_4_06 — Alpine and Arctic Ecology: Life at the Extremes
Alpine and Arctic ecosystems — the treeless biomes occurring above the climatic treeline in mountains (alpine) and above ~60–70°N latitude where mean temperature of the warmest month is <10°C (arctic) — share fundamental
ZB_3_19 — Permafrost Methane
Permafrost — permanently frozen ground maintained at or below 0°C for at least two consecutive years — underlies approximately 22% of the Northern Hemisphere land surface (about 23 million km²), primarily across Siberia,
O_2_22 — Carolina Bay Anomalies
The Carolina bays are a collection of approximately 500,000 shallow, elliptical depressions concentrated along the Atlantic Coastal Plain of the southeastern United States, from New Jersey to northern Florida, with the h
O_2_08 — Weathering, Erosion, and Deep Time Landscape Evolution
Weathering (the in-situ breakdown of rock and minerals) and erosion (the transport of weathered material by water, wind, ice, and gravity) are the fundamental surface processes that, operating over deep time (millions to
O_5_01 — Permafrost, Cryosphere, and Frozen Time Capsules
Permafrost — permanently frozen ground covering approximately 25% of the Northern Hemisphere's land surface — is simultaneously a geological archive, a biological deep freeze, and a ticking carbon time bomb. Ice cores ex
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