The Navajo Nation is a self-governing territory of 27,425 square miles in northwestern New Mexico, northeastern Arizona, and southeastern Utah. The formation, a volcanic plug, rises 1,600 feet above a barren desert plain south of the San Juan River. Shiprock’s Navajo Name Shiprock is called Tse Bit? a? i in Navajo, which means “rock with wings” or simply “winged rock. ” The formation figures prominently in Navajo Indian mythology as a giant bird that carried the Navajo from the cold northlands to the Four Corners region.
Shiprock, when viewed from certain angles, resembles a large sitting bird with folded wings; the north and south summits are the tops of the wings. Shiprock’s Name The formation was originally called The Needles by explorer Captain J. F. McComb in 1986 for its uppermost pointed pinnacle. The name, however, didn’t stick since it was also called Shiprock, Shiprock Peak, and Ship Rock, which is its name on a map from the 1870s, because of its resemblance to 19th-century clipper ships. The town nearest to the rock mountain is named Shiprock.
The Legend of Shiprock Shiprock is a sacred mountain to the Navajo people that figures prominently in Navajo mythology. The primary legend tells how a great bird carried the ancestral Navajos from the far north to their current homeland in the American Southwest. The ancient Navajos were fleeing from another tribe so shamans prayed for deliverance. The ground beneath the Navajos became a huge bird that transported them on its back, flying for a day and a night before landing at sunset where Shiprock now sits.
The Term Paper on Sedimentary Rock 2
Sedimentary rock formation begins with igneous, metamorphic, or other sedimentary rocks. When these rocks are exposed at the earth’s surface they begin the long slow but relentless process of becoming sedimentary rock. Weathering All rocks are subject to weathering. Weathering is anything that breaks the rocks into smaller pieces or sediments. This can happen by the forces of like wind, rain, and ...
Dine, the people, climbed off the Bird, which rested from its long flight. But Cliff Monster, a giant dragon-like creature, climbed onto the Bird’s back and built a nest, trapping the Bird. The people sent Monster Slayer to combat Cliff Monster in a Godzilla-like battle but in the fight the Bird was injured. Monster Slayer then killed Cliff Monster, cutting off his head and heaving it far to the east where it became today’s Cabezon Peak. The monster’s coagulated blood formed the dikes, while grooves on the Bird drained the monster’s blood.
The Bird, however, was fatally injured during the great battle. Monster Slayer, to keep the bird alive, turned the bird to stone as a reminder to the Dine of its sacrifice. More Navajo Legends About Shiprock Other Navajo myths tell how the Dine lived on the rock mountain after the transport, descending to plant and water their fields. During a storm, however, lightning destroyed the trail and stranded them on the mountain above sheer cliffs. The ghosts or chindi of the dead still haunt the mountain; Navajos ban climbing it so the chindi are not disturbed.
Another legend says Bird Monsters lived on the rock and ate humans. Later Monster Slayer killed two of them there, turning them into an eagle and an owl. Other legends tell how young Navajo men would climb Shiprock as a vision quest. Shiprock is Illegal to Climb Shiprock is illegal to climb. There were no access problems for the first 30 years of its climbing history but a tragic accident that resulted in a death in late March, 1970 caused the Navajo Nation to ban rock climbing not only on Shiprock but on all Navajo lands.
Prior to that, Spider Rock in Canyon de Chelly and The Totem Pole in Monument Valley were closed in 1962. The Nation announced that the ban was “absolute and unconditional,” and was due to “the Navajo’s traditional fear of death and its aftermath, such accidents and especially fatalities often render the area where they occur as taboo, and the location is sometimes henceforth regarded as contaminated by evil spirits and is considered a place to be avoided. ” Climbers have, however, continued to climb Shiprock since the ban, often obtaining permission from the local grazing holder.
The Term Paper on Igneous Rock
This article needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. (November 2012) Geologic provinces of the world (USGS) Shield Platform Orogen Basin Large igneous province Extended crust Oceanic crust: 0–20 Ma 20–65 Ma >65 Ma Igneous rock (derived from the Latin word ignis ...
Shiprock Geology Shiprock is the exposed neck or throat of a long-vanished volcano, which is the solidified feeder pipe of the volcano that erupted over 30 million years ago. At that time lava or molten rock came up from the earth’s mantle and was deposited on the surface of the mountain. Evidence suggests that the lava explosively interacted with water and formed what geologists call a diatreme or a carrot-shaped volcanic vent. The United States Geological Survey calls Shiprock “one of the best known and most spectacular diatremes in the United States. The neck is composed of various kinds of volcanic rocks, some deposited in cracks in the diatreme after it cooled. Erosion later removed the upper layers of the volcano as well as surrounding sedimentary rocks, leaving the erosion-resistant rock mountain behind. Shiprock’s volcanic plug as seen today was deposited between 2,000 and 3,000 feet below the earth’s surface. Shiprock’s Dikes Besides Shiprock’s unusual size as a volcanic plug, it is also famed for numerous rock dikes that radiate out from the main formation.
The dikes formed when magma filled in cracks during volcanic eruptions and then cooled, forming the long distinctive rock walls. Like Shiprock, they gained prominence when the surrounding bedrock was stripped away by erosion. Three main dikes radiate out from the main formation, to the west, northeast, and southeast. Rock Formations on Shiprock Shiprock is composed of fine-grained volcanic rocks, which solidified in the vent as the volcano cooled and became inactive.
Most of the formation is a combination of a pale yellowish tuff-breccia, composed of angular rock fragments welded together. Dark dikes of basalt were later intruded into cracks, forming dikes in the formation as well as a few large areas like the Black Bowl on the northwest side of Shiprock as well as the radiating long dikes. Much of the exposed rock surfaces on Shiprock are crumbling and often unsuitable for climbing. Extended crack systems are rare and are hard to climb with rotten brittle rock. Robert Ormes Attempts Shiprock
The Essay on When There Is A Sudden Breaking Of Rocks Within
When there is a sudden breaking of rocks within the earth or an explosion, wave like energy travels through the earth and is recorded on seismographs. These are called seismic waves and they are of two types: body waves and surface waves categorized into different kinds. What we will be discussing are body waves; there are two types of body waves: primary waves (P waves) and secondary waves (S ...
Monolithic Shiprock, towering above the desert floor, was one of the main objectives of American climbing in the 1930s. In the late 1930s there was a rumor that a $1,000 prize awaited the first ascent team but all failed, including Colorado climber Robert Ormes who attempted Shiprock several times with Dobson West in 1936. Besides Shiprock’s technical difficulties, the big problem for Ormes and other suitors were routefinding dilemmas. After a failed attempt, Ormes decided that the best route to the summit was via the Black Bowl.
In 1937 Ormes returned with a larger experienced team but while attempting a crack system up a basalt dike, took a 30-foot leader fall when a foothold broke. A single piton held the fall, bending it in half. Two days later Ormes returned with Bill House, who had held his fall, but the pair was unable to solve the difficulties of what is now called the Ormes Rib since they didn’t know aid climbing techniques and again turned back. Robert Ormes later wrote of the attempts and his fall in an article entitled “A Bent Piece of Iron” in the Saturday Evening Post in 1939.
First Ascent in 1939 In October, 1939, a crack California team composed of David Brower, John Dyer, Raffi Beayan, and Bestor Robinson drove from Berkeley, California to Shiprock with the intention of becoming the first to climb the formation. On the morning of October 9, the climbers ascended the west face to a prominent notch called the Colorado Col below the scene of Ormes’ fall. The team searched for an alternative to Ormes’ Rib, finding a circuitous passage which required rappelling down the east side of the notch, then traversing across the northeast side of the peak.
After three days of climbing (returning to the base each night) they surmounted the Double Overhang and climbed the bowl above to the base of the final problem on the Middle Summit. Bestor Robinson and John Dyer aid climbed up a steep crack system below the Horn by pounding pitons into the expanding crack. At the top of the pitch, Dyer lassoed the Horn and hand-drilled an expansion bolt, their fourth one, for a belay anchor. Another difficult pitch lead to easier climbing and the untrodden summit of Shiprock. Bolts Used for First Time in American Climbing
The Essay on The Second Coming Vs Things Fall Apart
The book Things Fall Apart , by Chinua Achebe , is very similar to the poem , "The Second Coming" by William Butler Yeats. A comparison of "The Second Coming" to Things Fall Apart will show many corresponding aspects between both of these literary masterpieces. Seeing the line "Things fall apart" in the poem , Achebe makes an outstanding association. At this point in time he says to himself, "I ...
Shiprock is the place where the first expansion bolts were placed in American climbing. The party carried a handful of bolts and hand drills to protect rock sections that had no cracks that would accept pitons. Four bolts were placed-two for protection and two for anchors. In the 1940 Sierra Club Bulletin, a magazine published by The Sierra Club, Bestor Robinson wrote, “Lastly, and with some concern over the mountaineering ethics of our decision, we included several expansion bolts and stellite-tipped rock drills.
We agree with mountaineering moralists that climb by the use of expansion bolts as taboo. We did believe, however, that safety knew no restrictive rules and that even expansion bolts were justified in order to secure the firm anchorage that would present a serious fall from imperiling the lives of the entire party. ” Besides bolts, the party brought 1,400 feet of rope, 70 pitons, 18 carabiners, two piton hammers, and four cameras.
