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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