Archive: Maguiresbridge

Explore every Emerald Archives article connected with Maguiresbridge.

31570–31561 BCE

31567 BCE

BIRM-166 at Maguiresbridge

Around 31,567 BCE, Ireland cannot be described through yearly events, but through fragmentary environmental evidence. Derryvree, near Maguiresbridge, Fermanagh, preserves freshwater sediments dating broadly to this period, indicating ice-free, open, wet tundra with severe periglacial conditions. Ireland’s ice cover and coastlines were changing regionally as the British–Irish Ice Sheet developed and low sea levels altered connections with Britain. Castlepook Cave in Cork documents varied Pleistocene fauna, though its remains span long intervals and cannot form a single scene. No secure contemporary human settlement exists. A possibly butchered reindeer bone offers only provisional evidence of brief human activity during this era.

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31630–31621 BCE

31624 BCE

Maguiresbridge and Castlepook

Approximately 31,624 BCE, Ireland lay within the unstable Marine Isotope Stage 3 cold period, not a precisely identifiable historical year. Inter-till deposits at Derryvree, Greenagho and Hollymount in Fermanagh show episodes of ice-free freshwater tundra later overridden by glaciers. Plant and insect remains indicate open, treeless, periglacial environments, while fluctuating sea levels and ice complicated access to the island. Castlepook Cave in County Cork preserves bones of mammoth, reindeer, giant deer, bears, wolves and hyaenas, reflecting intermittent cold-adapted fauna. A possibly cut-marked reindeer bone suggests, but does not prove, Upper Palaeolithic human activity. No institutions or political history are known.

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31640–31631 BCE

31633 BCE

Beneath Maguiresbridge Drumlin

Around 31,633 BCE, Ireland lay in an unstable Late Pleistocene interval before the Last Glacial Maximum. Evidence cannot reconstruct a single year or island-wide landscape, but sediments at Derryvree in Fermanagh record freshwater wetlands between ice advances, supporting tundra-like vegetation and insects. Other sites confirm episodic ice-free conditions. Castlepook Cave in Cork preserves a long-accumulated fauna including mammoth, giant deer, reindeer, predators and smaller cold-adapted animals. A cut-marked reindeer bone may indicate Upper Palaeolithic butchery, but human presence remains unproven without associated tools or settlement evidence. The record depicts environmental change, wildlife and possible transient human access, not named societies.

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31670–31661 BCE

31663 BCE

Maguiresbridge Bogbean Pool

31,663 BCE is a modern label for a Middle Midlandian MIS 3 interval, not a recoverable historical year. At Derryvree, County Fermanagh, freshwater deposits between glacial tills record a cold, non-glacial wetland of sedges, mosses, bogbean, insects and open tundra vegetation, later sealed by ice. Related Fermanagh sites indicate complex regional climatic change. Castlepook Cave, County Cork, preserves bones of mammoth, giant deer, reindeer, predators and other cold-adapted fauna, though deposits span long periods. A marked reindeer bone may suggest human butchery, but cannot prove settlement. These archives reveal Ice Age environments, while political, cultural and economic history remains unknown.

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31667 BCE

The Maguiresbridge Interstadial

At approximately 31,667 BCE, Ireland lay in the climatically unstable Late Pleistocene, not a historical year with identifiable communities. Freshwater deposits beneath later glacial till at Derryvree, County Fermanagh, and Greenagho indicate ice-free local basins supporting tundra-steppe vegetation, pools, sedges, mosses, dwarf willow and juniper. Cave remains at Castlepook, County Cork, demonstrate varied cold-climate fauna, including reindeer, mammoth, giant deer and predators, though not all were contemporary. A possibly stone-cut reindeer femur may indicate brief Upper Palaeolithic human activity, but remains disputed and proves neither settlement nor hunting. Expanding ice buried, disturbed and erased evidence before the Last Glacial Maximum.

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31680–31671 BCE

31673 BCE

The Maguiresbridge Freshwater Lens

Circa 31,673 BCE, Ireland cannot be described through a dated event, but through a variable Marine Isotope Stage 3 environment. At Derryvree, near Maguiresbridge, freshwater silts between glacial tills preserve evidence of ice-free, treeless periglacial wetlands, with mosses, sedges, grasses, herbs and juniper. Castlepook Cave in Cork records mammals, including mammoth, reindeer, giant deer, bears, hyaenas, wolves and lemmings, across many millennia, demonstrating ecological links with north-west Europe. A marked reindeer bone may indicate human butchery, but remains contested. No settlements or social institutions are known. Together, these archives reveal dynamic, intermittently habitable landscapes, later overridden by advancing ice sheets.

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31678 BCE

The Maguiresbridge Freshwater Series

31,678 BCE is a modern label for a broad Late Pleistocene interval, reconstructed from environmental evidence rather than recorded events. At Derryvree, County Fermanagh, freshwater deposits between glacial tills reveal an ice-free or largely ice-free, periglacial tundra landscape with pools, sedges, mosses and sparse vegetation before renewed glaciation. Castlepook Cave, County Cork, preserves MIS 3 remains of reindeer, giant deer, mammoth, hyaena and other fauna, though accumulated over time. A possibly cut-marked reindeer bone suggests brief human presence, but occupation remains unproven. These archives show dynamic, regionally varied Ice Age Ireland, later extensively reshaped by expanding ice sheets over millennia.

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31810–31801 BCE

31802 BCE

The Maguiresbridge Silts

Around 31,802 BCE, Ireland lay within the climatically unstable Marine Isotope Stage 3, not a date capable of supporting annual history. At Derryvree near Maguiresbridge, freshwater silts, mosses, sedges and Arctic insects between till layers record a cold, treeless, locally ice-free interval. Comparable northern deposits show repeated glacial advances and retreats. Castlepook Cave preserves remains of cold-adapted fauna, including reindeer, giant deer, mammoth and predators, accumulated over varied periods. A possibly tool-marked reindeer bone suggests, but cannot prove, brief human presence. Evidence supports environmental change and animal occupation, while rejecting claims about contemporary Irish society, settlement or continuous human ancestry.

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