Philip England recognizes that the goal of science is to understand nature’s processes, the essence of understanding is the ability to predict from general conditions, bringing understanding to Joe Sixpack requires simplicity, and simple understanding can be expressed most clearly by algebraic expressions, or scaling laws. With Steve Richardson and later with Margaret Moore (and Carslaw and Jaeger), he showed how erosion affects crustal temperatures. With Alan Thompson, he showed how the thermal history of buried rock, and therefore metamorphism, depends on rates and depths of burial and exhumation. With Tim Holland (and Archimedes), he revealed the conditions required for ultrahigh-pressure rock to return to the surface in the face of subduction shear. With Greg Houseman, Dan McKenzie, and Leslie Sonder, he combined the two major forces that limit elevations of deforming lithosphere—friction or viscosity and gravity—into one dimensionless number, the Argand number. With this simplification, he then explained many aspects of the large-scale distribution of active deformation, like present-day velocities and strain rates, rotations about vertical axes, crustal thicknesses, and subcrustal seismic anisotropy. With Stephen Bourne and Barry Parsons, he showed how slip rates on faults can scale simply with the spacing between faults. With Richard Katz and Catherine Wilkins, he showed how the positions of volcanoes at subduction zones depend simply on the subduction rate and the dip of the downgoing slab. In a counterintuitive, homely analogy, the faster you thrust ice beneath your bed, the warmer you will be (provided that the movement of your ice forces a circulation of warm water above it)! Not just a theorist who has reduced nonlinear differential equations to algebraic scaling laws, he has also led efforts to obtain new data, especially GPS measurements. Finally, as a public servant, he organized a multidisciplinary program, Earthquakes Without Frontiers, to study both the science and the societal impacts of earthquakes in continental regions, where they have taken their greatest toll but are least well understood.
Philip England has brought simple understanding to a wide variety of thermal and mechanical processes in the solid Earth. Young scientists could benefit from examining how he chooses, then poses, and finally solves problems.
—Peter Molnar, Department of Geological Sciences, Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder
Measurements of surface heat flux from boreholes of the NIED Hi‐net network of seismometers are used to determine temperature and shear stres...