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45 results for "continental drift" — page 1 of 3
R_4_17 — Biogeography & the Wallace Line: Continental Drift, Island Life, and Distribution Puzzles
Biogeography — the study of the geographic distribution of organisms, both past and present — has been central to evolutionary biology since Alfred Russel Wallace (1823–1913) identified the sharp faunal boundary between
O_2_03 — Plate Tectonics, Continental Drift, and Deep Earth
Plate tectonics — the theory that Earth's outer shell (lithosphere) is divided into rigid plates that move, collide, and separate atop a convecting asthenosphere — is one of the great unifying theories of modern science.
O_2_19 — Expanding Earth Theory
The expanding Earth hypothesis proposes that the planet has significantly increased in radius (and possibly mass) over geological time, with continental drift and ocean basin formation being consequences of this expansio
M_4_13 — Earth Crustal Displacement: Hapgood's Theory and Its Legacy
Earth crustal displacement (ECD) — the hypothesis that the Earth's lithosphere can shift as a relatively intact shell over the underlying asthenosphere, rapidly relocating the geographic positions of continents relative
ZF_1_03 — Seafloor Spreading, Plate Tectonics and Marine Geology
The discovery that the ocean floor is not ancient and static but young, dynamic, and continuously recycled revolutionized Earth science in the 20th century. Seafloor spreading — proposed by Harry Hess (1962) and confirme
ZB_4_01 — Biogeography and Island Biology
Biogeography — the study of the geographic distribution of organisms — was one of Darwin's and Wallace's most powerful lines of evidence for evolution and remains central to modern biology. Alfred Russel Wallace identifi
G_4_18 — Biogeography and Ancient Distribution Patterns
Biogeography — the study of the spatial distribution of organisms across the planet, both present and past — is one of the most powerful frameworks for understanding Earth history, evolutionary processes, and the mechani
O_2_12 — Great Rift Valley: Continental Splitting and Hominid Cradle
The East African Rift System (EARS) — commonly called the Great Rift Valley — is one of Earth's most geologically dramatic and scientifically significant features: an active continental rift zone stretching approximately
H_2_16 — Dissident Scientists: Careers Destroyed by Heterodox Views
The history of science includes numerous cases of researchers whose careers were damaged, marginalized, or destroyed because they advanced ideas that contradicted the prevailing scientific paradigm — ideas that were, in
H_2_06 — Successful Paradigm Shifts in Archaeology: Cases Where Orthodoxy Was Wrong
The history of science contains well-documented cases where firmly held orthodoxies were overturned by new evidence, often after decades of resistance from established authorities. Thomas Kuhn's The Structure of Scientif
F_4_08 — Mu and Lemuria — Lost Continent Theories
Mu and Lemuria are two related but distinct "lost continent" traditions that have profoundly influenced alternative history, esoteric thought, and popular culture. Lemuria originated as a legitimate biogeographic hypothe
ZF_1_13 — Continental Shelves: Submerged Geography and Ice Age Coastlines
Continental shelves — the shallow, gently sloping underwater extensions of continental landmasses — represent some of the most biologically productive, economically valuable, and archaeologically significant terrain on E
E_3_04 — Doggerland and Sundaland — Drowned Continental Shelves
Doggerland and Sundaland represent two of the most significant landmasses lost to post-glacial sea level rise, together encompassing hundreds of thousands of square kilometers of habitable terrain that was progressively
F_4_25 — Doggerland: Europe's Submerged Landscape
Doggerland is the name given to the now-submerged landmass that once connected Britain to continental Europe across what is now the southern North Sea. During the Last Glacial Maximum (~26,500–19,000 years ago), when sea
M_5_23 — Post-Glacial Flooding and Submerged Archaeological Landscapes
Between the Last Glacial Maximum (LGM, c. 26,500–19,000 years ago) and approximately 6,000 years ago, global mean sea level rose by approximately 120–130 m, drowning continental shelves that had been habitable land. The
M_1_17 — Underwater City Discoveries (Dwarka, Yonaguni, Pavlopetri)
The discovery and investigation of submerged archaeological sites — cities, harbors, temples, and infrastructure now lying beneath coastal waters due to post-glacial sea level rise, tectonic subsidence, or local geologic
ZF_3_09 — Ocean Currents and Human Migration Patterns
Ocean currents have shaped human migration, trade, and cultural exchange throughout prehistory and history — functioning as both highways and barriers that profoundly influenced which populations could reach which coastl
ZF_3_01 — Sea-Level History: Glacial Cycles, Meltwater Pulses, and Coastal Archaeology
Sea level has varied by over 120 meters between glacial and interglacial periods, repeatedly reshaping coastlines, exposing and flooding continental shelves, and creating or destroying land bridges that directed human mi
ZF_5_20 — Wallace Line: Biogeographic Boundary and Deep-Time Distribution Patterns
The Wallace Line is a biogeographic boundary running through the Malay Archipelago, separating the fauna of Asia (Sunda Shelf) from that of Australasia (Sahul Shelf). First identified by Alfred Russel Wallace during his
ZF_5_08 — Coastal Geomorphology: Erosion, Beaches, and Barrier Islands
Coastal geomorphology is the study of landforms at the interface of land and sea — a dynamic zone shaped by the constant interaction of waves, tides, currents, wind, rivers, geology, biology, and increasingly by human ac
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