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mixed with blood, transmitted through the arteries to the brain where they are separated from the blood and stored in the channels and ventricles of the brain for use under the direction of the soul. Thomas Willis (1684) published a fairly accurate description of nerves and his theories about convulsive diseases. He conjectured that animal spirits formed in the brain produce motions by explosive action. When this explosive action is excessive, convulsions and mental disease result. After Isaac Newton (1642 1726) published his Philosophiae Naturalis Principia Mathematica in 1687, the concept of animal spirits was rede ned as a vital gravitational force (elan vita). The Italian anatomist Luigi Galvani (1737 1798) reported that electrical energy is propagated along the nerves and generates muscular movement, a discovery that nally led to the abandonment of the belief that animal spirits move through tubular nerves. However, the doctrine of animal spirits was not wholly replaced as a physiological explanation for sensation and action and the notion of animal electricity (vis nervosa) replaced that of animal spirits. Clarke and Jacyna (1987) comment as follows:

EPILOGUE VoIP-based global communications are a reality today for international calling among both employees of multinational corporations and residential PSTN customers. National long-distance carriers and international calling service providers are deploying this service on a limited scale for both multinational corporations and residential customers. In PSTN networks, the availability of a dial tone is guaranteed within 300 msec of picking up the handset in 95% of the instances, as mentioned in the LSSGRs; call setup delays are at most 3 sec and 10 sec for local and international calls, respectively, after the last digit is entered; and toll quality (i.e., a MOS score of 4.0) of voice transmission is almost always guaranteed. It may be di cult to support cost-e ectively the traditional PSTN-grade availability, reliability, and security for calling services to hundreds of thousands of customers using IP-based network elements for call control and signaling and media transmission. Both competitive and traditional telephone service providers, however, are rolling out VoIP-based national and international calling services using many innovative solutions, including (a) using one-for-one redundancy for VoIP call servers or call managers and other critical network elements in a POP, (b) clustering of IP-PSTN MGWs and other network elements to provide shared protection of services, (c) peering of network nodes and links to maintain an acceptable level of QoS for packet transmission, and (d) active and passive monitoring of network and nodal resources such as transmission and callprocessing capabilities so that the toll quality of voice transmission can be guaranteed for the admitted voice connections. We expect to see further proliferation of these types of networking and service protection techniques for VoIP and related services in the next-generation public and enterprise networks within 10 years.

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It is as well to appreciate that the natural landscape is not an utterly passive determinant of groundwater ow patterns. Many landforms are themselves sur cial expressions of processes of erosion (and, less commonly, sedimentary deposition) intimately associated with groundwater ow systems (e.g. Baker et al. 1990). The science of landforms is geomorphology. Thorough explorations of the interrelations between geomorphology and hydrogeology have already been published elsewhere (LaFleur 1984; Ford and Williams 1989; Higgins and Coates 1990; Brown 1995); here we will restrict ourselves to brie y appraising the roles of those geomorphological features which form the principal boundaries to most natural groundwater ow systems. Recharge areas As 2 makes clear, the literal starting points for the circulation of almost all groundwaters are those locations in which direct or indirect recharge occur, i.e. recharge areas. Classically, recharge areas are thought of as the hilltops in districts underlain by aquifers. While there is no denying that much recharge does occur beneath hills developed on the outcrops of aquifer materials, recharge will as readily occur

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