In centuries past, when winters in London were colder, sections of the river Thames would sometimes freeze so solidly that �frost fairs,� events featuring ice-skating and open-air markets, could be held on the surface�
Introduction
Permafrost is defined as soil that remains frozen for more than two years. At elevations less than 304.8 m (1000 ft.), it is frequently encountered north of latitude 60. It may also be...
A Retrospective on Early Analysis and Simulation of Freeze and Thaw Dynamics
Study of Frozen Cloddy Soils Properties as a Road Embankment Material in Permafrost Regions
Permafrost Prethawing in Farming, Mining, and Civil Engineering
Mitigation Options to Reduce Thaw Instability Hazard at the Denali Park Mile Post 45 Landslide
Effect of Dissolved Solids on Freeze-Thaw Conditioning
Fighting Frost Problems in New York State Pavements
Reducing Damage to Low Volume Asphalt-Surfaced Roads, and Improving Local Economies: Update on Variable Tire Pressure Project
Large Aircraft Operations at Small Airports: When Can Heavier-than-Design Aircraft Use Thin Frozen Pavements?
Concept of Ensuring the Serviceability of the Roadbed of the Berkakit-Tommot-Yakutsk Railway on Sections of Very Icy Permafrost
Breakup on the Upper St. John River
Measurement of the Pore Size Distribution of Geomaterials Using Conductometric Phase Transition Porosimetry
Effects of Low Temperature on Concrete Strength
Rigid Insulation to Reduce Foundation Embedment
Ice Storms, Trees and Power Lines
Ice and the Wire Systems of a Transmission Line
Structural Analysis: Kachemak River Culverts
Treatment by Freeze-Thaw of Membrane Concentrates
Improved Spring Load Restriction Guidelines Using Mechanistic Analysis
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