8. A Volcanic Heritage Geoscape
The second Storied Rocks case involves a large red cinder cone volcano (Scrugham Peak), on top of a high flat basalt lava flow (Buckboard Mesa), located in the center of a large caldera (Timber Mountain) in a broader region of volcanic events (
Figure 9) (Christiansen and Lipman 1977). The edge of the caldera is largely formed by high mountains that were either pushed up during the formation of the main Timber Mountain Caldera or from subsequent volcanic eruptions.
Much of this southern Nevada and eastern California region is managed by US federal agencies such as the Department of Energy (DOE) as the Nevada Test Site (NTS), the US Nelis Air Force as the UTTR, National Parks Service (NPS) at Death Valley, and the Bureau of Land Management (BLM). This analysis was largely funded by the DOE NTS, but three decades of our research in the Amargosa River hydrological system has mutually informed our knowledge of Native American story rocks and environmental adaptations over thousands of years.
The findings presented in this analysis largely derived from the first 14 years of an annual government to government consultation between the Department of Energy Nevada Test Site managers and 17 Native American Tribes. That official consultation was a partnership between the DOE and the Tribes who annually met to discuss ethnographic studies, agency EIS needs, and tribal heritage preservation desires. The tribes organized themselves as the Consolidated Group of Tribes and Organization (CGTO) as to provide a uniform response to the NTS land managers. The consultation is best understood through two documents: American Indians and The Nevada Test Site (Stoffle, Zedeño, and Halmo 2001) and the PhD dissertation on the topic by David Halmo (2001).
Figure 10 is a satellite image of the key geological and heritage places in the caldera: clockwise they area (1) Black Mountain, (2) Water Bottle Canyon, (3) Buckboard Mesa, (4) Forty Mile Canyon, (5) Shoshone Mountain, and (6) Timber Mountain. Lower left in the image is Death Valley. The climate is diverse today but was a massive wetland and forested area in the late Pleistocene and early Holocene. Death Valley in wetter times was filled with water forming the deep Lake Manley, and Forty Mile Canyon was a stream feeding into the Amargosa River. Ancient ecology influenced traditional Native American perceptions and uses of the land.
The high mountains surrounding the caldera drain into a deep canyon created by Forty Mile stream (
Figure 11). Water flowing from this canyon is a major tributary of the Amargosa River which flows into Death Valley. During the Pleistocene, all of these places experienced so much rain that the Amargosa River filled Tecopa Lake along its course and Death Valley at its terminus with what is called Lake Manley. Indian people have been in the Amargosa River hydrological system for at least 37,000 years. During this period, this massive drainage was filled with megafauna, abundant flora, and many topographically distinct features. It remained so throughout the late Pleistocene and during much of the Holocene when the climate became dryer and colder so many animals and plants could no longer occupy the region, but Native Americans adapted and remained. Most of the Storied Rocks in the Timber Mountain Caldera are centered at Buckboard Mesa.
One of the most striking characteristics of Storied Rocks on the Nevada Test Site are their abundance in the Timber Mountain Caldera, especially on and around Buckboard Mesa (
Figure 12). According to the Native Americans, places of great significance for vision questing and ceremony were localized around Buckboard Mesa and Scrugham Peak because these were volcanic areas (Stoffle et al. 2001; Stoffle, Van Vlack, Arnold 2005; Stoffle et al. 2006; Zedeño et al. 1999: 155). These volcanic features are a perceived source of power and are seen as the geographic and sacred center of the area. The power emanated from the caldera and Buckboard Mesa provided and furnishes power to all associated Earth elements. It is not surprising to them, therefore, that Storied Rock sites such as Buckboard Mesa (north and south) and upper Forty Mile Canyon are located near this center.
Historically documented areas to the northeast, such as
Wunkiakuda near Ammonia Tanks (Steward 1938: 94 -95), are now understood from ethnographic interviews as a ceremonial area focused on a tonal canyon, a massive solar calendar area, a rights of passage area with bow trees, and a massive white stone portal (Stoffle, Van Vlack, and Arnold 2005). The trails indicated in red on Map (
Figure 13) are largely formerly pilgrimage trails to Wunkiakuda.
The information in
Table 1 is a summary of tribal assessments of the purpose of Storied Rock at ten locations in the central caldera (see
Figure 13). Buckboard mesa has hundreds of rock piles located near the peckings. These are documented stone constructions that have been interpreted as Vision Questing
cairns. Each
category of purpose identified in the table involves a question on the Rock Art interview instrument. The responses are organized by gender. The Storied Rock markings, some of which are illustrated later, varied widely among the ten locations both in terms of design, and number of markings. Some places like Cot Cave had only a few markings while the Buckboard Mesa had hundreds including many vision questing cairns. Stones, even if they were neither pecked nor painted, were moved and modified at all locations.
Table 1 presents the findings from ethnographic interviews with tribal representatives. Their responses are organized by (1) Story Rock Location, (2) Kinds of Uses, and (3) Gender of the Respondent (Zedeño et al. 1999).
The ten Storied Rock places in
Table 1 were each culturally understood by the tribal representatives interviewed at these locations. The interview forms structured only the kinds of responses, but open-ended knowledge sharing was common. Clearly, some places were for ceremony while others were to teach other ethnic groups or youth who were being prepared for medicine, spiritual communication, or leadership. Knowledge was sought in places like the Power Rock but not nearby at Eagle Rock. The responses were thoughtful with up to three hours devoted to understanding (which involved talking with the Storied Rocks location) and interviewing at each location. Almost always there were different understandings for women and men. These data clearly support the theory that the Storied Rocks are all about the place where they are located.
8.1. Buckboard Mesa Pilgrimage Trail
The Pilgrimage Trail to Buckboard Mesa could be termed as it is in the map above the Trail to Scrugham Peak, given it is this volcanic peak is the highest point in this central portion of the Timber Mountain Caldera. Another pilgrimage trail, however, leaves the main trail and goes to the top of Shoshone Mountain. Both pilgrimage trails begin and end at the same location.
Figure 14 presents a map view of the Story Rock sites profiled in this analysis. Relationships between the center point at Buckboard Mesa and surrounding Story Rock areas studied by tribal elders vary in a number of important ways such as (1) geology, (2) size, and (3) distance between the starting point at Tippipah Spring and at the mesa center. Interestingly they are all on the pilgrimage path or geotrail (Stoffle et al. 2001; Stoffle et al. 2006; Zedeño et al. 1999). There is no proximal Story Rock sites located away from the two divergent pilgrimage trails, which further argues that these are geotrails; that is, designed to ceremonially connect geologically special places.
A formal Rock Art interview form was developed with the CGTO in the late 1990s to help achieve systematic data collection during Storied Rocks studies (Zedeño et al. 1999). It was used again during the Shoshone Mountain study (Stoffle et al. 2001), the Water Bottle Canyon study (Stoffle, Van Vlack and Arnold 2005), and the Timber Mountain study (Stoffle et al. 2006). Thirty tribally appointed representatives who were interviewed during seven field studies conducted in 1997 and presented the 1999 Story Rock study report. Each subsequent study had tribal representatives. Questions reflected culturally important topics developed during successful interviews with representatives of consulting tribes. The ethnographic field interviews also were guided by rock art site documentation by professional archaeologists working at the Desert Research Institute, University of Nevada, Las Vegas.
Tribal representatives participated in designing the methods by expanding the range of site studies, the questions asked at each site, and the time spent interviewing at each location. These changes in methodology occurred as tribal representatives better understood the focus of Storied Rocks studies. Interviews occurred with different tribal representatives and were often conducted during seven field sessions. The University of Arizona research teams were guided by three professionals with PhDs in anthropology and supported by a PhD in archaeology from Desert Research Institute. Each representative was afforded a confidential interview with a trained ethnographer and given the right to review and approve the summation of their interview before it was reported to the NTS DOE land managers.
The Buckboard Mesa Pilgrimage Trail extends from (1) Tippipah Spring as a ceremonial starting and ending point (see
Figure 14). The pilgrim trail goes next to (2) the first Geoglyph, then to (3) the Doctor Rock, next to (4) the Mushroom or “Eagle” Rock, and to (5) upper Forty Mile Canyon at Rice Grass Village and the large “Map Pecking” of the Buckboard Mesa area. From here the whole surrounding Upper Forth Mile headwater area is documented as being for ceremonial use. This area includes (6) the second geoglyph area, (7) the volcano basalt boulders, access to (8) the top and sides of Buckboard Mesa and Scrugham Peak. All Storied Rock places along the geotrail have ethnographically identified portals to other dimensions. These portals, however, differ in structure, protocols, and where they take the pilgrim.
8.2. Geosiste 1: Tippipah Spring
Tippipah Spring is a strong permeate source of water largely derived from Shoshone Mountain to the southeast of the spring (
Figure 15). As a reliable source of water in what is an extremely arid caldera today, the spring was a center of Native American activities. While a few Native people lived at the spring full time, it is better termed a Ceremonial Support community rather than an agricultural community. The latter were located in Oasis Valley to the west, further south along the Amargosa River, along the Las Vegas River to the southeast, and along the edge of the Colorado Plateau. Primary agricultural rivers located here were the Pahranagat or White River, Moapa or Muddy River,
Tonaquint or Santa Clara River, Mukuntuweap or Virgin River), and Colorado River. Each irrigated agricultural community along these rivers would have had at least 300 residents according to observations in the mid 1700 to 1800s.
Residents at the Ceremonial Support community, as was the pattern throughout the west, central America, and the Andes of Peru (Bauer and Stanish 2001). Their responsibility was to take care of ceremonial paraphrenia, ensure that ongoing prayers are conducted, and provide food for pilgrims. Ceremonial paraphrenia are event and location specific and are stored in shallow rock shelters which are often walled up for protection. These paraphrenia cannot be taken back to residential agricultural communities because people there should not be exposed to their power. A hidden ceremonial paraphrenia storage area was found near Tippipah Springs in the mid-20th Century despite the site being lost to Native control during the middle 1800s when a series of trails were converted into a wagon road, a stage stop was established, and predatory miners occupied all spring during the 1904 gold rush of Oasis Valley. The ebb and flow of non-Native water users opened opportunities for the traditional Native people to return to the spring and the area for ceremonial activities. Portions of area just north of the caldera however were better suited as regions of refugee such as Water Bottle Canyon, which was used for this purpose when USGS surveyors marked its location in 1906 placing the valley and Native trails to it on the first USGS map of the area.
Tippapah Spring does not contain Storied Rocks. It has a different function, being the place where pilgrimages to story rock geosites begin and end their journey. Other springs in the broader area have ceremonial functions.
8.3. Geosite 2: The First Geoglyph
The first geosite after leaving
Tippapah Spring is a Geoglyph. This site has been extensively studied over time because of its charismatic features and being near Tippapah Spring which is a central watering and stopping location (
Figure 16). Closer to the NTS, several geoglyphs are located in the Mojave Desert, and in fact, many are found near the Colorado River with Blythe Intaglio being the most famous. This geoglyph was discovered in 1931. The Blythe Intaglio depicts several characters, one of which is
Mastamho, the Creator of the Earth, and two mountain lions that helped him. Sacred ceremonies were held here to honor
Mastamho (BLM 2005).
Geoglyphs were considered very important to the Indian people along the Colorado River who often use the designs in connection with religious ritual, dancing on the lines as if they were paths. This is an important point because geoglyphs and trails are connected. In fact, geoglyphs in the southwestern United States are thought to forge a spiritual link to trails (von Welhof and Casey 1987).
The Geoglyph One site impressed Wheeler, an early archaeologist, so much he identified it as a ceremonial area. He further described the patterns of cobbles as appearing to be creating walkways leading into circles, perhaps for dances or other rituals. During his excavations of the site in 1940, Wheeler uncovered yellow ochre, or Limonite, which is a very important paint source. The source of yellow ochre is located near this area and was probably brought in by Indian people to use in ceremonial activities. Artifacts such as chert and obsidian drills, bifacial scrapper, silicified volcanic knife, ground stone, pottery, and fire hardened juniper sticks were found and removed from the site by Wheeler (Wheeler 1940, Winslow 1996:154-159).
Based on our new interviews in the Timber Mountain study (Stoffle et al. 2006) it was concluded that after leaving the settlement at Tippipah Support Village and Spring, pilgrims traveling both Puha Path I and Puha Path II would have arrived at the Geoglyph One. This site is located 3.5 miles from Tippipah Spring in a small and heavily dissected valley. It would have been the next logical stop along Puha Path I before reaching the Doctor Rock, and also along Puha Path II, which diverges from the shared route and leaves the Geoglyph One for the Ceremonial Rock Shelters.
Another elder noted that the geoglyph is connected through the volcanoes, through a power spot, by having everything you would need. They would have cleaned themselves at the hot spring in Beatty before coming up here. It is a well-used area. They had to spend a lot of time together and they came here to do that.
This idea [for the geoglyph] could have come from far away. The idea here is that someone can see it from above. It was to talk to those above. The [geoglyph] could be seen from the top of the volcanoes to the south. You could see the area and know about it. We need to go to the top to see what alignment with Scrugham Peak. People could put themselves in a trance and go quietly from one area to another go miles and just be there very quickly. That is an Owens Valley story from an old person who was told it by his grandfather. They could travel without using much energy. There were people used for sending messages. Most of the people who traveled could do that. The mind can do many things. It is capable if you use it right.
According to one elder, the geoglyph area could have been used while people were en route to another location. People would stop here on the way to other places. Many respondents suggested that this area was a stopping point on the way to other sites connected to this one.
8.4. Geosite 3: The Doctor Rock
After passing through Geoglyph One, Indian people traveling along Puha Path I would have walked 2.93 miles to come to this location (Stoffle et al. 2005). The Doctor Rock geosite contains several cultural features: (1) two large boulders covered with peckings lie by the roadside at the bottom of a drainage; (2) a small rock shelter and artifact scatter in front of it are across from the boulders on the south side of the road above the wash, and are marked by cairns; and (3) a large flat boulder with a hole in its center and a smaller rock staked under it are located on the ridge top just above the petroglyph panels (
Figure 17).
For this analysis, only the Doctor Rock is being discussed because it is defined as a portal for doctoring and travel of religious and political leaders.
There is evidence that the Doctor Rock itself has been moved to this location according to tribal representatives (
Figure 18). The component materials of the Doctor Rock are not otherwise present at the location. The Doctor Rock is located on a high point at the junction of two intermedial streams. Another stone panel that is both large and fully covered with peckins (6 feet by 5 feet)is located down slop from the Doctor rock on the side of the hill. This panel was uniformly and independently interpreted by the oldest tribal elders as the location of intertribal meeting from cultural groups throughout the region. A small structure across from the Doctor rock was interpreted as a place for storing ceremonial materials that were too powerful to be taken back to normal residential areas.
Once it was moved to this location it was perched onto a large stone (
Figure 19). The large stone itself is covered with desert varnish indicating that it too was moved to this location to become a part of the ceremonial components of the Doctor Rock. The portions of the supporting stones that are covered with desert Varnish are under the Doctor Rock and thus not exposed which would have been needed for the desert varnish to occur.
8.5. Geosite 4: Mushroom (Eagle) Rock
Eagle Rock, also called Mushroom Rock, is a large, isolated, welded tuff boulder named after its shape (
Figure 20). The site is along Forty Mile Wash at the base of a ridge extending from Shoshone Mountain and close to the Doctor Rock site, which is 0.9 miles to the west (Zedeño et al. 2005). The top of the formation contains petroglyphs; associated archaeological remains are found underneath the petroglyphs and in the rock’s immediate vicinity (Jones and Drollinger 1997: 26, 28). Evidence of this site’s use along Puha Path I is suggested by a rock ring, ground stone, and many artifacts, both prehistoric and historic scattered beneath it (Zedeño et al. 1999). Because of the mushroom-like shape of the boulder, it likely provided shelter. Like the Doctor Rock site, pilgrims would have used Eagle Rock as a prayer and preparation area. Interpretation of the site and peckings were difficult for the elders in as much as the USAF used it as a target for fighter plane shooting practice. These actions broke a major portion off and disrupted the integrity of the peckings.
In 1997, Indian tribal representatives deemed the Eagle Rock very sacred and an ethnic marker (Zedeño et al. 1999). The site was interpreted as a place for medicine and the performance of ceremonies. Tribal representatives also believed it was a teaching site for young boys to learn about the ways of medicine.
In summary, of 22 elder interviews conducted at this geosite, Eagle Rock was used to teach young boys how to clean out water tanks, how to perform medicine, and how the patterns of the stars will guide a person in their travels (Stoffle et al. 2006, Zedeño et al. 1999). It was also found that it was a landmark through which people would have recognized and talked about the land. The shape of the rock is like that of an eagle, which is a sacred bird. Also here are large amounts of obsidian and extensive rock pecking covering most surfaces. Obsidian could have been left by pilgrims as offerings along their journey. These features and artifacts indicate that this is a culturally special place that was used for medicine and ceremony.
8.6. Geosite 5: Upper Forty Mile Canyon
Upper Forty Mile Canyon is steep sided area defined by its headwater at the northwest slope of Buckboard and by the northeast margin of the Timber Mountain resurgent dome. The photos (
Figure 21) below are from the headwater of the watershed looking southwest towards Shoshone Mountain. The edge of Buckboard Mesa is left with a Red-Tailed Hawk flying overhead. The right side is the edge of the resurgent dome. The bottom of the canyon is white sand. A rock shelter called Big George Cave is visible near the eastern side of the wash approximately halfway to the headwater divide to the north.
By 1999 DRI had undertaken systematic field research that greatly expanded knowledge of the extent, content, and significance of this area (Zedeño et al. 1999: 47). Based on diagnostic projectile points and pottery, they estimate that the area has been used for the last 9,000 years (Jones 1996: 15). About 440 boulders displaying almost 3,000 individual petroglyphs are found in various concentrations throughout the site.
At the entrance to the headwaters of Upper Forty Mile Canyon is a small spring and a large volcanic boulder with large peckings on one face (Figure W). Elder interpretations of the entrance boulder peckings were largely in agreement that it was a map of the area and its culturally important places.
Figure 21.
Boulder at Entrance to Upper Forty Mile Canyon with Map Pecking to right.
Figure 21.
Boulder at Entrance to Upper Forty Mile Canyon with Map Pecking to right.
Given the location and style of the entrance, bolder peckings elders identified the rock as a map guiding pilgrims to the ceremonial places in Upper Forty Mile Canyon. Key interpretations were provided by Clifford Jake. He often used an old style High Chief language which was understood by the study linguist David Saul. In the upper right portion of the pecking is a snake image and later in this analysis we discuss Forty Mile Canyon as being either a snake or created by a snake.
8.7. Geosite 6: Second Geoglyph
The second geoglyph is located near the map rock and spring and is visible in two images in
Figure 22. The geoglyph was interpreted as functionally the same as the one near Tippipah spring. This one however lacks the long apparent entranceways and consists of a circular rock alignment with two appended semicircles (Zedeño et al. 1999: 47). The circles are clearly visible and do not appear disturbed (Jones 1996: 27). One Pinto point and one Rosegate point were recorded in this area (Jones 1996). Desert Side -notched projectile point and an unidentified dart also found in this area suggest dates of 1,200 BP and 1,500 BP, respectively (Jones 1996: 25).
8.8. Geosite 7: Basalt Boulders With Peckings
In Upper Forty Mile Canyon there are hundreds of boulders, each with a pecking and most with a rubbed grinding area (
Figure 23). The stimulus for the peckings were generally interpreted as being associated with vision questing. There was, however, some discussion of whether or not the visions were acquired in Forty Mile Canyon or were recorded there after being experienced on Buckboard Mesa and Scrugham Peak.
Rock cairns on the mesa and peak were interpreted as a record of visions, but a discussion was open as to whether or not the visions pecked on the boulders below in the canyon could actually serve as a portal for another person to the same vision. Many boulders had parallel dots on them which have been widely interpreted as evidence of an entopic state. The questions remain as to whether this dream state is an experience in the same body and place or something occurring in another dimension. There was no clarity on this issue, however a number of boulders had modified holes in them. Such holes have been documented in a number of studies involving portals as where pilgrims enter another dimension by placing their finger covered with red paint in the hole.
Figure 24.
Basalt Boulder With Peckings.
Figure 24.
Basalt Boulder With Peckings.
Figure 24.
Basalt Boulders with Peckings.
Figure 24.
Basalt Boulders with Peckings.
Figure 25.
Basalt Boulder with Modified Hole for Entrance into Another Dimension.
Figure 25.
Basalt Boulder with Modified Hole for Entrance into Another Dimension.
A summary of upper Forty Mile Canyon Storied Rock locations, that is based on about 35 formal interviews and many informal discussions document that all Native American tribal elders felt a strong ancestral, cultural, and historical relationship with upper Forty Mile Canyon (Zedeño et al. 1999:55)
When asked why the petroglyphs were made and how were they were used, tribal elders offered the following answers, in order of frequency:
* Ceremony
* To seek knowledge or power
* To map resources
* To communicate with spiritual beings
* To communicate with other Indian people
* To teach other Indian people
* To pay respects
* To mark their territory
At the most general level of abstraction, the Storied Rocks in this area were viewed as places where people of different ethnic groups would have come to conduct ceremonies. People would have known how to read the entrance map to know where resources occur as well as for proper sites for religious activities.
8.9. Geosite 8: Buckboard Mesa and Scrugham Peak
The tribal representatives generally agreed that the top of Buckboard Mesa and associated Scrugham Peak were places where visions were sought and found by Native specialists (Figure M). The mesa and peak are directly observable volcanic features and thus would have been sought out for their special energy and spiritual powers (Stoffle et al. 2005, Stoffle et al. 2024, Zedeño et al. 1999).
These areas are the primary destination of the geotrail from Tippipah Spring; however, geosites along the trail were at least their own ceremonial places in and of themselves. The ethnographic data documents the use of rock piles or cairns to make places where vision quests were successfully conducted. These cairns line the rim of Buckboard Mesa and along the flank of Scrugham Peak. Associated with the basalt rim are peckings that either expand the stories of the cairns or convey another related story altogether. Buckboard Mesa and Scrugham Peak are considered one place by Indian people and are connected through ceremonial activity.
The mesa rim is a 66 to 99 foot high basalt cliff extending around the entire circumference of the mesa. Located there are natural ledges and rock shelters where Desert Research Institute archaeologists found evidence of previous Indian use (Pippin and Henton 1991). Additionally, archaeologists have recorded artifacts and built features located on top of and along the southwest rim of the escarpment directly overlooking Big George’s Cave. These resources include a 3,300 foot horizontal alignment of rock cairns on the edge of the mesa, spatially associated with boulders displaying rock art, large rock art panels on the escarpment below the edge, a milling stone, a possible rock wall, lithic scatters. Cairns are small piles of rocks spaced at approximately regular intervals and extend 1,650 feet in each direction of the natural staircase to the mesa surface (Jones and Drollinger 1997:20).
Buckboard Mesa placed in a geological context is unique (Lutton 1968). It is a massive basalt lava flow located between the east and west headwaters of Forty Mile Canyon. It largely emerged during a single volcanic flow. It is 5.5 miles long in a generally trending northwest direction. It is about 2.5 miles at its widest and narrows to a point in the south. Emerging from the surface of the mesa top is a 400-foot-high cinder cone called Scrugham Peak (
Figure 26).
The mesa basalt probably emerged during the final stage of caldera subsidence in the Pliocene or Pleistocene. Surrounding the mesa are deposits of sandstones, breccia, and water worked pumice, all being indicators of an extensive fluviatile environment in the Forty Mile flanks of the emerging mesa (Lutton 1968).
Scrugham Peak is composed of red cinders which are scattered over the basalt, some of which emerged during the eruption of the cinder cone. The cinder cone contains magma dikes, and its top depression was filled in with magma creating cumulo dome (Lutton 1968). This is an important feature of the peak in as much as the basalt in the peak has given it stability in the face of atomic tests on the mesa.
A critical variable in the Native American representative’s interpretation of the mesa and peak is a series of nuclear and high-explosive cratering experiments that were conducted in the basalt capping Buckboard Mesa by the U. S. Atomic Energy Commission Nevada Test Site from 1960 through 1966. It is understood that some of the vision quest cairns were collapsed as a result of these explosions. The map in
Figure 27 illustrates the latticework of roads on the surface of the mesa.
A general consensus expressed by one tribal representative is that: they would have camped below the mesa top but then came up here to do their spirit-seeking. They had to be in a group. The seeker needs helpers. There were no women in these camps. The rock piles were where they stayed to seek their vision and get medicine. The people who received the medicine made the rock piles (
Figure 28 and
Figure 29). The later ones would use the same piles, and it was reused for thousands of years. All the peckings were made for the same reason - this is a power place.
One of the panels that had a profound impact upon the Native American representatives was the “three legged” anthromorph (
Figure 30). Representatives strongly believed that it is linked to vision questing ceremonies. The panel was also interpreted as representing a spirit helper, perhaps a lizard. Pilgrims might have interacted with that panel and acquired a spirit helper to assist them in the last segment of their journey along Puha Path I to the top of Scrugham Peak.
The sacredness of the mesa top and rim is represented by other peckings such as the scratches just under the mesa edge (
Figure 30). This pecking was further interpreted as powerful because it is home to Indian Tobacco that grew out of the cliff face.
Below the edge of Buckboard Mesa, youth, probably mostly boys, were taught to talk with, work with, and form together tools made from obsidian nodules. Large areas of such nodules occur just to the northeast of Buckboard Mesa where fist size obsidian nodules can be found in abundance.
During the 1996 NAGPRA consultations, Native American representatives commented on a traditional use feature at the northern base of Buckboard Mesa (
Figure 31). At this location, there are a series of rock shelters that were associated with an obsidian nodule tool stone source area or quarry and extensive lithic scatters. Numerous rock shelters associated with petroglyphs indicate that this area was used in prehistoric times. Seven obsidian points were selected from this site. Interpretations given for this place exemplify how activities such as raw material procurement, tool making, and hunting are viewed by Indian elders as sacred, all because the ceremonies involved were close to the petroglyph. This is a power place located on Buckboard Mesa. Native American representatives associated this area as a place where boys would learn to knap obsidian and make arrow points as part of rites of passage ceremonies (Stoffle et al. 1996).
Along the edge of the mesa, near the obsidian training location, are peckings. A portion of one panel is in
Figure 32 As a part of this panel is another rattlesnake image and a snake symbol. The pecked circles were interpreted as entrances into other dimensions.
Tribal representatives studying and interpretating these locations said they represented locations with artifacts that should be returned to the tribes under the Native American Graves Protection and Repatriation Act (NAGPRA). They qualify as both objects of cultural patrimony and sacred objects that should not be removed because they are part of an ongoing ceremony as a link between the ceremonial participants the living volcano.
8.10. Scrugham Peak
This volcanic cinder cone mountain was the destination site for those traveling for a vision (
Figure 33). Native American representatives believed that seeking visions and learning medicine songs and practices occurred on the peak. They would have used Puha acquired during previous visits to the various petroglyph panels. Numerous rock cairns are located on the western side of the mountain (
Figure 34) and these cairns were used in ceremonial activities by the pilgrims, who would ascend to the top of Scrugham Peak and stay for a number of days and nights until their vision had been achieved.
The ceremonial experience occurring on the top of Scrugham Peak involves being 400 feet higher in elevation and having a broad view of the surrounding landscape (
Figure 35). In general, higher elevations are significant components of vision quests but can also be critical to ceremonial leaders who are sending prayers to other locations. The rock cairns on Scrugham Peak are similar to those elsewhere. The presence of circular rock walls however on the peak and scattered along the rim of Buckboard Mesa led the tribal elder believe different kinds of ceremonies were involved at these differently marked Story Rock locations.
The notion that Scrugham Peak involved (and may involve again) cultural activities on a volcano that is located on top of another volcano did not pass without mentioning the significant of having the power of each volcano added to the other. In general, powerful living beings whether plant, animal, or geological are attracted to one another and see each other out.
8.11. Origin Stories and Geoscapes
American Indian consultants offered additional comments regarding the existence of songs and song trails associated with upper Forty Mile Canyon (Zedeño et al. 1999). This information suggests that there may be a geotrail that ties different songs to specific locations in the area. Indeed, one Southern Paiute elder recalled having received a song - -his song -- during a visit to the NTS area. Similarly, at least one oral tradition, which refers to Snake as the creator of Forty Mile Canyon, also indicates the existence of storyscapes.
According to a Western Shoshone elder, the origin story of Towahonupi or Forty Mile Canyon was created when Snake went through this place, traveling from Oasis Valley to Beatty, and then to Bear Mountain, where he is resting now. When Snake was traveling, he made the canyon. So, the canyon is named after him. Snake is tokoa in Western Shoshone. There are many petroglyphs here that talk about Snake. That is why this place is so dangerous. People should not stay here too long or disturb the area. This Shoshone origin story was also collected during the Yucca Mountain research. Water babies and Mountain Sheep also have resource-specific stories that serve an important role in tying places and resources to larger cultural landscapes.