Tag Archives: artwork

Shiprock Formation, New Mexico

The rock formation known as Shiprock, in the New Mexico desert, is a monadnock, or formation that rises alone out of a flat or gently sloping plain. It stands very close to the Four Corners region of the United States, the only place where four states meet at the same point.

Genuine Curteich-Chicago “C.T. Art Colortone”


The description states:
234 — SHIPROCK, NEW MEXICO
(SHIP OF THE DESERT)
This shaft of rock rising to a height of 1864 feet above the plain, dominates the landscape for many miles. The beautiful play of the changing lights on the rock are a source of delight to all who behold it.
From certain positions the resemblance to a “Windjammer” is very marked, hence the name “Ship of the Desert.”
–The rock is made up of volcanic material which cooled in the central pipe of a volcano, and was left behind when the rest of the volcano eroded away.
This postcard likely dates from the 1940s.

Flowering Yucca Plant, New Mexico

This is an artist’s rendition of the Yucca plant in flower, a common plant in the desert southwest. Its full range extends from Guatemala in the south to Alberta, Canada in the north.

Genuine Curteich-Chicago “C.T. Art Colortone”


The description states:
The YUCCA, a plant peculiar to the deserts of the Southwest, is variously called Spanish Bayonet, Lamparas de Dios (Lamps of the Lord) and “Soapweed”. It is found in New Mexico, Texas, Arizona, and California. The roots are used by the Indians as soap, while the leaves are used for basket making. It has been adopted as the State Flower of New Mexico.
–This plant has become a popular ornamental plant and is used in residential areas and as decoration around businesses in urban areas.
This card likely dates from the 1940s.

Owl Rock, Albuquerque, New Mexico

This image shows a rock formation along the historic U.S. Route 66 west of New Mexico, which with some imagination has come to be called Owl Rock.

Genuine Curteich-Chicago “C.T. Art Colortone”


The description states:
116–OWL ROCK ON HIGHWAY U. S. 66 ABOUT 40 MILES WEST OF ALBUQUERQUE, N. MEX.
–This formation is still visible from the roadway that now passes by it, which has been upgraded and slightly relocated over the intervening decades.
This card likely dates from the 1940s.

Continental Divide Vista, New Mexico

This card has a view of the Great Basin and Range at the point where the water flows either east to the Gulf of Mexico, or west to the Pacific Ocean, known as the Continental Divide.

Genuine Curteich-Chicago “C.T. Art Colortone”


The description states:
10 — CONTINENTAL DIVIDE
The Great Continental Divide extends from Alaska through the Western United States, Mexico, Central America and South America to Patagonia. From this “Divide” the water (streams) run definitely east or west.
We cross this Highway “66” just about 115 miles west of Albuquerque and 30 miles east of Gallup, N. M. This spectacular view of the Red Rocks is from the village at the Divide.
–Highway 66 is a reference to the legendary U.S. Route 66 which originally ran from Chicago, Illinois to Santa Monica, California, but it has been replaced almost entirely by the later Interstate Highway System roads.
This card likely dates from the 1940s.

Volcanic Lava, New Mexico

This image shows a deposit of volcanic lava, known locally as malpais, which was formed from the now extinct volcanoes in the San Francisco Peaks region of New Mexico.

Genuine Curteich-Chicago “C.T. Art Colortone”


The description states:
No. 21 — VOLCANIC LAVA
In some remote period Mt. Taylor, the San Francisco Peaks, and other mountains in the Southwest were volcanic and belched forth great masses of black lava and cinder which still remain in its hardened state as it was after calling off ages ago.
Great areas, locally called Malpais (lava) may be seen from the highway near Tularosa and Carrizozo or as we pass Grants and Ice Caves, also near Flagstaff, Arizona.
–The lava is found throughout the Arizona and New Mexico desert regions. Because it is extremely irregular and poor soil, it is considered useless badlands. There is a national monument by a similar name, the El Malpais National Monument, which features extensive examples of this formation located in New Mexico.
This postcard likely dates from the 1940s.

Ocotillo Cactus, New Mexico

This is an image of a type of plant native to the Sonora and Chihuahua Deserts. The Ocotillo cactus is not a true cactus.

Genuine Curteich-Chicago “C.T. Art Colortone”


The description on the back states:
277–OCOTILLO CACTUS
Forqueiria Splendens, also called Candlewood, Coach-whip Vine Cactus and Jacob’s Staff, at time appears as dry sticks only. The rainy season causes it to flame with slender, brilliant red panicles of bloom. Many Southwestern hillsides are literally covered with this spiny shrub.
–The stems are hard enough to provide a kind of living fence when planted or grown in sufficient density, and are also harvested for walking sticks.
This image likely dates from the 1940s.

Rock Cliffs, Laguna, New Mexico

This is a vista of the Acoma rock cliffs and the foot trail that winds among them. The Acoma  Pueblo is a mesa community, accessible only by the foot trail.

Genuine Curteich-Chicago “C.T. Art Colortone”


The description states:
148 – ROCK CLIFFS AND FOOT TRAIL AT
ACOMA, “THE SKY CITY”
SOUTH OF HIGHWAY U.S. 66,
NEAR LAGUNA, N. M.
Coma Pueblo, a seventy acre Mesa, 350 feet above the Plains is the oldest continuously inhabited place in the United States. This view shows the foot trail ascending to the village, the only access to the Plateau and gives an idea of the steep formation of the Gibraltar Rock.
–This image likely dates from the 1940s.

Women’s and Men’s Dormitories, Western State Teacher’s College, Kalamazoo, Michigan

This dual image shows the two main residential buildings which housed students at the Teacher’s College in Kalamazoo, Michigan. By this time the name had been changed to a more explicit description of the school’s purpose. Two buildings were essential as it was not acceptable to have men and women living in the same buildings while students.

Genuine Curteich-Chicago “C.T. Art Colortone”


There is no description on the back of this card.
These buildings have been renovated and repurposed over the century, and the Women’s Dormitory, erected in 1938 is now an administration building, after a 1992 renovation.  The Hall of Men appears to now be called Spindler Hall.
Since the school was renamed the Western State Teacher’s College in 1927 until 1941, this image likely dates from 1938 or 1939.

Western State Normal School Admin Building and Science Hall, Kalamazoo, Michigan

This card has images of both the main Administration building, top, and the Science Hall, bottom, which served to train teachers for the public school system in this area of Michigan.

H. H. Hamm, Toledo, Ohio


There is no description on the back of this card.
Of particular interest is the object and sloping pathway to the right of the Administration building. This was a funicular railway, and the passenger car is shown at the bottom waiting to take passengers up the steep slope from the lower to the upper campus. The railway was built in 1907 and operated until 1949.
The Administration building was erected in 1905, and the Science Hall in 1915. They are also known as East and West Hall, on the original eastern campus.
This image likely dates from the 1920s.

Western State Normal School Gymnasium, Kalamazoo, Michigan

This image is of the college gymnasium building on the original campus of the Western State Normal School, now the campus of Western Michigan University.

H. H. Hamm, Toledo, Ohio


There is no description on the back of the card.
These Normal Schools were established to provide training for public school teachers throughout the state. As time passed, they either closed, or in the case of Western, evolved into more comprehensive training and research institutions.
As this building was erected in 1925, and the institution was known as a Normal School only until 1927, it is certain this card dates from the mid-1920s.