Like all the more western subspecies, parietalis is strikingly different from typical sirtalis in having conspicuous red markings. The relationship between the two was early recognized. Several of the other subspecies were originally described as distinct species. Coluber infernalis Blainville, 1835; Tropidonotus concinnus Hallowell, 1852; Eutainia pickeringi [Baird and Girard, 1853]; and others now considered synonyms eventually came to be recognized as conspecific with Thamnophis sirtalis. [Ruthven] (1908:166-173) allocated all western sirtalis to either parietalis or concinnus, the latter including the populations of the northwest coast in Oregon, Washington and British Columbia.
Subsequent more detailed studies by later workers with more abundant material led to the recognition of some subspecies that Ruthven thought invalid and led to the resurrection of some names that he had placed in synonomy. [Van Denburgh and Slevin] (1918:198) recognized infernalis as the subspecies occurring over most of California and southern Oregon, differing from more northern populations in having more numerous ventrals and caudals and a paler ground color. [Fitch] (1941:575) revived the name pickeringii for a melanistic population of western Washington and southwestern British Columbia, restricting the name concinnus to a red-headed and melanistic population of northwestern Oregon, and restricting the name infernalis to a pale-colored population in the coastal strip of California.
These changes left most of the populations formerly included in concinnus and infernalis without a name, and [Fitch] (op. cit.) revived Thamnophis sirtalis tetrataenia (Cope) to apply to them. However, [Fox] (1951:257) demonstrated that the type of T. s. tetrataenia came from the San Francisco peninsula (rather than from "Pit River, California" as erroneously stated in the original description) and that the name was applicable to a localized peninsular population rather than to the wide-ranging far western subspecies, which he named T. s. fitchi. The range of fitchi includes California west of the Colorado and Mohave deserts (except for the narrow strip of coast occupied by infernalis and tetrataenia), Oregon except the northwestern part, Washington east of the Cascade Range, most of British Columbia, extreme southeastern Alaska (occurring farther north than any other terrestrial reptile of North America) and parts of Idaho.
Neither [Fox] (1951) nor [Fitch] (1941) defined the eastern limits of fitchi or discussed its relationship to the subspecies parietalis. [Wright and Wright] (1957:849) stated: "Fitch ... did not even mention the big scrap basket form parietalis, from which he pulled T. s. fitchi (old tetrataenia). That comparison remains to be made, and the east boundary of fitchi and the west boundary of parietalis are still nebulous." We have undertaken to define better than has been done before the ranges of parietalis and fitchi and to list the diagnostic characters separating these two subspecies. Freshly collected material of both has been compared. At the time of his 1941 revision the senior author had never seen a live or recently preserved specimen of parietalis.
Discontinuity of Range
Wherever it occurs at all, the common garter snake is usually abundant. Because of its diurnal habits and the concentration of its populations along watercourses, it is not likely to be overlooked. There are few, if any, remaining large areas in the United States where herpetologists have not carried on field work. It may be anticipated that certain rare and secretive species will still be found far from any known stations of occurrence, and seeming gaps in the ranges of these species will eventually be filled. But for the common garter snake the negative evidence provided by the lack of records from extensive areas should be taken into account in mapping the range.
Most large collections of garter snakes contain misidentified specimens. The diagnostic differences in color and pattern are often obscured, especially if the specimens are poorly preserved. Many specimens deviate from the scalation typical of the form they represent, and key out to other species. Isolated records should therefore be accepted with caution. A case in point is Colorado University Museum No. 46, from Buford, Rio Blanco County, Colorado, originally identified by [Cockerell] (1910:131) as Thamnophis sirtalis parietalis. This specimen, and another, now lost, from Meeker in the same county seemingly served as the basis for mapping the range of sirtalis across the western half of Colorado, for there seem to be no other records from this part of the state. However, a re-examination of the specimen from Buford shows it to be an atypical individual of another species, T. elegans vagrans. A specimen of T. radix haydeni (Col. U. Mus. No. 3165) was the basis for [Maslin's] (1959:53) record of parietalis in Baca County on the north fork of the Cimarron River in southeastern Colorado. [Brown] (1950:203) has mentioned the difficulty of defining the range of sirtalis in the southern Great Plains because of misidentifications of the similar T. radix.
The range of the common garter snake has never been adequately mapped in the Rocky Mountain and Great Basin states. Recent general works ([Smith], 1956:291; [Wright and Wright] 1957:834; [Stebbins] 1954:505; [Conant] 1958:328) which have shown maps of the over-all range of sirtalis, differ sharply as to the extent of its distribution in Texas, New Mexico and Arizona, but all show its distribution as continuous over the more northern Great Basin and Rocky Mountain states. However, specimens and specific locality records from this extensive area seem to be scarce and some are based on early collections of doubtful provenance. Throughout this region the low rainfall, fluctuating and uncertain water supply, and general lack of mesic vegetation along many of the streams render the habitat rather hostile to garter snakes in general. Thamnophis elegans vagrans, highly adapted to conditions in this region and generally distributed over it, doubtless offers intensive competition to the species sirtalis wherever they overlap and perhaps constitutes a limiting factor for sirtalis in some drainage basins.
Convincing records of sirtalis are lacking from all of Colorado—except for those in the drainage basins of the South Platte, and the Río Grande east of the Continental Divide—from the eastern half of Utah (east of the Wasatch Range), from New Mexico except for the Río Grande drainage (with one record each for the Canadian and Pecos river drainages), from southwestern Wyoming (at least that part in the Colorado River drainage basin), from the western half of Oklahoma, and from Texas, except the eastern and extreme western and northern parts. The species occurs in Nevada only near that state's western and northern boundaries. The range is therefore much different than it has been depicted heretofore, with the populations living east of the Continental Divide widely separated from those to the west for the entire length of the Rocky Mountains south of the Yellowstone National Park region. The populations of northern Utah, southern Idaho, and Nevada, which have been considered parietalis are thus far removed from the main population of that subspecies to the east and are isolated from them by the barrier of the Continental Divide and arid regions farther west.
Although some of the records published for Thamnophis sirtalis are erroneous, being based on misidentifications of other species, various outlying records, including those in western Kansas, the Panhandle of Texas, and southeastern New Mexico probably represent localized relict populations that have survived from a time when the species was more generally distributed in this region. The population of T. sirtalis in the Río Grande drainage of New Mexico is geographically isolated and remote from other populations of the species. Except for a few isolated and highly localized populations the species is absent from the Republican, Smoky Hill, Arkansas, Cimarron, Canadian, Red, Brazos, Colorado and Pecos rivers and their tributaries west of the one hundredth meridian in the arid High Plains.