HARRINGTON] PLACE-NAMES 393 



ally curves around through grovea until, at La Cueva, it assumes an almost due 

 southerly direction. One or two more brooks increase its volume on the way, 

 descending directly from the mesa pedestal of the Jara Mountain [27:10], and 

 its name is changed from San Antonio to the Rio de San Diego [27: 13]. 



Just where the change in name occurs is indefinite. See [27:tj], 



[27:13]. 

 [27:12] South fork of San Diego Canyon [27:13]. 

 [27:13] (1) J cmez Put f of III u/iiiwdn/y, ' lioiliug water canyon' {PcUfv- 



fulu7iy,, see [27:8]; wdmy, 'canyon'). Since this is the canyon 



that has hot springs at various places in it, it is naturallj^ enough 



called 'boiling water canyon'. 



(2) Eng. San Diego Canyon. (<Span.). = Span. (3). 



(3) Span. Canon de San Diego, 'Canyon of Saint James'. =Eng. 

 (2). "Rio de San Diego ".1 



This canyon is very deep in its lower portion. The north fork 

 of its upper part is called San Antonio Can3'on, San Antonio 

 Creek; see [27:11]. 



[27:14] Jemez 'UfdgPi 'place where the one-seeded juniper trees are' 

 {'y, 'one-seeded juniper' ' Juniperus monosperma', akin to Tewa 

 hy,; fd 'to be at a place'; gPi locative, akin to Tewa gt). 



This is an ancient pueblo ruin, north of the Soda Dam [27:16] 

 and on the western side of the creek. It is separated from the 

 pueblo ruin [27:lo] by an arroyo. See [27:15]. 



[27:15] Jemez NqnifdgVi 'place where the cottonwood trees are' 

 {nqni 'cottonwood', species undetermined but probably Popukls 

 wislizeni; fd 'to be at a place'; gi^i locative). Niini is probably 

 cognate with Tewa nana 'aspen' but is not applied to the aspen. 

 "No-ny]sh'-a-gi"'.2 



This pueblo ruin is situated a short distance south of ruin 

 [27:14], from which it is separated by an arroyo. 



[27:1(3] The Soda Dam (pi. 14). This is what the place is called com- 

 monly in Eng. No Span, or Jemez name was learned. Bandelier 

 says of the place : 



In that gorge [San Diego Canyon], ice-cold soda springs issue near the river 

 bed, and a short distance above the bathing establishment [27:18] a huge cyl- 

 indrical dain traverses the stream, in which steaming currents and cold streams 

 flow parallel to each other, neither affecting the temperature of the others, 

 although only a few inches of rock separate them.' 



[27:17] (1) Jemez Giy,seii)dfdwa, said to mean 'pueblo at the hot place' 

 referring to Jemez springs [27:18] {(Jiy,sewd^ see [27:1S]; towd 

 'pueblo'). "Qicinzigua."^ "Qui-umzi-qua."^ 



' Bandelier, Final Report, pt. ii, p. 200, 1892. 



2 Hodge in Handbook Inds., pt. 2, p. 81, 1910. 



'Bandelier. op. cit.. pp. 202-203. 



<ZArate-Salmeron (ra. 1629) quoted by Bancroft, Native Races, i, p. 600, 1S82. 



sZdrate-Salmeron {ca. 1629) Rel., in Ltind o/ Sitnskine, Los Angeles, p. 183, Feb., 1900. 



