https://www.jstor.org/stable/1632410#metadata_info_tab_contents

This was published by the American Association for the Advancement of Science. At the end of this page, under the headline "special articles" is an article titled "Evidences of Glaciation in Southern Arizona and Northern Sonora". According to the author, the moraine is located between Nogales and Imuris:

"...along the Sonora Railway, south of Nogales, frequent exposures of material resembling in every way, except in its component rocks, that of the terminal moraine of New York and New Jersey. These exposure were between Nogales and Imuris... and exhibited sections of till and boulder clay with large angular rock fragments and the occasional partial stratification characteristic of various portions of the terminal moraine in the northeast"

"...there is, in the vicinity of Nogales, both in Arizona and in Sonora, and for a number of miles north and south of the national boundary, an area of some width in which land ice transportation has been operative and has resulted in the formation of morainal deposits of various types"

"Some ten miles north of Nogales rises... the Santa Rita Mountains... Within a mile or two of the southeastern base of the range passes the Sonora Railway, which here as in Sonora, by its numerous cuts and borrow pits, gives an opportunity to study the composition of a formation which has all the characteristics of a moraine deposit, but which, in the absence of sections, a casual observer might pass by as a terrane of volcanic material rotted in place..."

"...one recognizes at many points the rolling topography and pitted surface of a moraine. At one or two points are observed depressions, similar to those which in the north have been formed by tanant ice, surrounded by kame terraces and their concordant phenomena. One of these is just south of Huachuca Station."

"About three miles south of Nogales is a very extensive borrow pit, formed in the construction of the railroad, in which has been left a number of large rock fragments which are clearly of transported material. Among these, the writer noted several blocks of dark blue limestone which did not belong to the crystalline terrane beneath and which had evidently been transported some distance"

"[the extent of the glacial formations] are apparently limited to the vicinity of the higher mountain ranges. About twenty miles west of the Santa Rita Mountains, between Sopori and Arivaca, on the west of the Atascosa Range... which has a morainal appearance..."

"In northern Sonora, near the valley occupied by the railroad and between Nogales and Imuris, one sees near the mountain bases low benches which have been eroded into overlapping oblique ridges of which the material seems to be all of morainal character."

"In traveling eastward from Benson toward El Paso, at a few points, mountain masses were observed, rising from the desert plains, around the bases of which were slightly elevated benches corresponding in some measure to the bench of morainal material along the eastern base of the Santa Rita Mountains. Occasionally, also, the railroad cut through low rolling ridges of material morainal in structure and clearly not formed by sheet flood erosion"

"On the Rock Island Railway, about a mile southwest of Santa Rosa, N.M., near the southeastern bank of the Pecos River, is a train of rolling hills which show morainal structure in the railroad cuts"

"These observations lead to the conclusion that the quaternary history of some portion of this region is more complex than has been supposed. Clearly before the present period of arid climate and periodic sheet flood erosion was a time of low temperature and accumulated precipitation in the form of land ice which resulted in the formation of extensive deposits of rock debris around the bases of at least the higher mountain ranges. Climatic conditions limited the extent of these moraines so that the present desert basin areas, in many cases, remained unglaciated"

My crazy post about a pole shift, which you can read here helps explain why I think the cabal is interested in both Racine and other areas that feature terminal moraines. Every single place they have set up shop, without exception as far as I can tell, is on the edge of a terminal moraine. Allentown, for example, is only a few feet away from where a glacial advance terminated.