2021 Magazine
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2004 Central College Women's Track and Field
2003-04 SPRING CENTRAL COLLEGE PRESSBOOK Founded –1853 Enrollment –1,693 Affiliation –Reformed Church in America President – Dr. David Roe Membership – Iowa Intercollegiate Athletic Conference, National Collegiate Athletic Association, Division III Founded in 1853, Central College is a four-year coeducational liberal arts college of the Reformed Church in America. Located 40 miles southeast of Des Moines, Central offers its 1,659 students learning opportunities not only on the Pella campus, but international study sites in Hangzhou, China; London and Colchester, England; Paris, France; Eldoret, Kenya; Leiden, the Netherlands; Merida, Mexico; Granada, Spain; Carmarthen, Wales; and Vienne, Austria. Central is a member of the National Collegiate Athletic Association, Division III, and the lowa Intercollegiate Athletic Conference. Men compete in baseball, football, basketball, tennis, golf, wrestling, soccer, track and cross country while women compete in tennis, golf, track, softball, volleyball, cross country, soccer and basketball. Rugby is offered at the club level. The Kuyper Athletic Complex The Kuyper Athletic Complex is located at the corner of Independence Street and West Fifth Street in southwest Pella. The complex includes P.H. Kuyper Gymnasium (1970), H.S. Kuyper Fieldhouse (1987), A.N. Kuyper Field (1977), the baseball and softball fields (1978), Ryerson Golf Driving Range (2002), cross country course (2003), tennis courts (1992), soccer field (1992) and the Ron Schipper Fitness Center (1999). The complex also includes practice and intramural softball diamonds and football fields. Golf meets are held at the Bos Landen Golf Resort, two miles southwest of the campus on Highway T-15. Directory Sports Information Director (Interim) . Abby Gonzales Office. -
The Runner's Rite of Spring®
The Runner’s Rite of Spring® 1995 (April 9) women’s title in 54:28. A total of $35,000 was given to Chil- Pre-race speculation centered on the Kenyans cracking the dren’s Hospital, bringing the total charity contribution to 46:00 barrier for the first time. With world cross country over $140,000. runner up Ismael Kirui and 1994’s third place finisher Jos- phat Machuka as the top seeds, the stage was set (Sigei was 1998 (April 5) out due to injury). Race day dawned with no wind, although A new course featuring an out-and-back section on Rock temperatures were in the upper 50s and the humidity was Creek Parkway delighted the 5,800 finishers. South Afri- high. As expected, Kirui and Machuka went right to work, can Colleen DeReuck proved that the layout was fast as dropping further below world record pace with each pass- she shattered Rose Cheruiyot’s World Record for 10 Miles ing mile. Suffering from blisters, Machuka dropped off by of 51:39 — set in the 1995 race —with a scintillating 51:16 5 miles. Kirui slowed to a 4:41 ninth mile, but responded performance that placed her 23rd overall. (She would have with a 4:31 closer to smash Sigei’s year-old mark with a been the overall winner of the 1973 race!)DeReuck finished 45:38. Just over six minutes later Rose Cheruiyot of Kenya, over two minutes ahead of runner-up Marian Sutton of who had set a world 5K record a week before, collected the Great Britain. -
W.M.A.C. Snoshu-News
March 2006 Vol. 04 Issue 06. WW..MM..AA..CC.. SSNNOOSSHHUU--NNEEWWSS NOT WITH A BANG, BUT PRETTY DARNED CLOSE… There is a lot to be said for being “as flexible as Gumby.” That was several minutes faster than it should have been and I was mindset enabled Edward to lead his troops through seven series hanging on for dear life. Good thing this wasn’t the long races and two trail races in a winter that, at times, even wiped course! I truly don’t remember much about the race except that the big grin from the face of our fearless leader. In fact, this Bob pulled ahead and I surprised myself by keeping the winter was so discouraging that couch potatoes who normally momentum going and finishing better than I have all season. I complain about snow were feeling gypped. There’s only so remembered to smile for the camera and remained smiling even much November grayness a body can take. So that’s one good when Tippi threatened to bite my fingers. thing anyway. Perhaps next year it won’t be only us and the school kids who get excited about snow. The next day of this final grand slam weekend was Curley’s at Thunderbolt. Of all the transferred races we have had this And, looking back, while the snowshoe season was frustrating, season, substituting one black diamond course for another was a especially for the race directors, with the November/December perfect match. Andy Keefe and I carpooled and since we were snow we did get off to an earlier start than last year. -
Volume 66 Issue 1 Winter 2021
Preservation By David Blacker, Executive Director From the Director DVNHA One of the biggest highlights of visiting Death Valley National Park or Ash Meadows National Wildlife Refuge is seeing and maybe getting a photo of a desert bighorn sheep. You see the desert bighorn in our logo, a strong and majestic animal with iconic large curling horns, but your chance of seeing one of these incredible creatures is shrinking. Surprisingly the biggest reason is not climate change, but the spread of an invasive species that dominates and destroys their water sources and bullies them out of their historic range. In the economic downturn of the early 2000s, people stopped adopting burros and the Bureau of Land Management (BLM) pens filled up. A growing unchecked burro population began to grow and spread. I began to hear reports of sightings in Panamint Valley and the Nevada Triangle back in 2005. Now there are herds occupying Butte Valley, Skidoo, Wildrose, and southern areas of the park. Everywhere burros appear, the impact is predictable. First they seize control of the local water source, trampling or eating the native vegetation. Being very territorial, they use their size and aggressive nature to chase off any competition. Once burros move into a water source, bighorn sheep will not use it. Our partners at NPS are working diligently to reduce and remove invasive burros from the park. They have partnered with Peaceful Valley Donkey Rescue to roundup and adopt out burros from Death Valley. Burro numbers increase by 20-30% a year, so more than 750 burros need to be rounded up annually to stay ahead of reproduction. -
Death Valley National Park
COMPLIMENTARY $3.95 2019/2020 YOUR COMPLETE GUIDE TO THE PARKS DEATH VALLEY NATIONAL PARK ACTIVITIES • SIGHTSEEING • DINING • LODGING TRAILS • HISTORY • MAPS • MORE OFFICIAL PARTNERS T:5.375” S:4.75” PLAN YOUR VISIT WELCOME S:7.375” In T:8.375” 1994, Death Valley National SO TASTY EVERYONE WILL WANT A BITE. Monument was expanded by 1.3 million FUN FACTS acres and redesignated a national park by the California Desert Protection Act. Established: Death Valley became a The largest national park below Alaska, national monument in 1933 and is famed this designation helped focus protection for being the hottest, lowest and driest on one the most iconic landscapes in the location in the country. The parched world. In 2018 nearly 1.7 million people landscape rises into snow-capped mountains and is home to the Timbisha visited the park, a new visitation record. Shoshone people. Death Valley is renowned for its colorful Land Area: The park’s 3.4 million acres and complex geology. Its extremes of stretch across two states, California and elevation support a great diversity of life Nevada. and provide a natural geologic museum. Highest Elevation: The top of This region is the ancestral homeland Telescope Peak is 11,049 feet high. The of the Timbisha Shoshone Tribe. The lowest is -282 feet at Badwater Basin. Timbisha established a life in concert Plants and Animals: Death Valley with nature. is home to 51 mammal species, 307 Ninety-three percent of the park is bird species, 36 reptile species, two designated wilderness, providing unique amphibian species and five fish species. -
Newsletter 2020
NEWSLETTER 2020 POOVAMMA ENJOYING TRANSITION TO SENIOR STATESMAN ROLE IN DYNAMIC RELAY SQUAD M R Poovamma has travelled a long way from being the baby of the Indian athletics contingent in the 2008 Olympic Games in Beijing to being the elder FEATURED ATHLETE statesman in the 2018 Asian Games in Jakarta. She has experienced the transition, slipping into the new role MR Poovamma (Photo: 2014 Incheon Asian Games @Getty) effortlessly and enjoying the process, too. “It has been a different experience over the past couple of years. Till 2017, I was part of a squad that had runners who were either as old as me or a couple of years older. But now, most of the girls in the team are six or seven years younger than I am,” she says from Patiala. “On the track they see me as a competitor but outside, they look up to me like a member of their family.” The lockdown, forced by the Covid-19 outbreak, and the aftermath have given her the opportunity to don the leadership mantle. “For a couple of months, I managed the workout of the other girls. I enjoyed the role assigned to me,” says the 30-year-old. “We were able to maintain our fitness even during lockdown.” Poovamma reveals that the women’s relay squad trained in the lawn in the hostel premises. “It was a change off the track. We hung out together. It was not like it was a punishment, being forced to stay away from the track and the gym. Our coaches and Athletics Federation of India President Adille (Sumariwalla) sir and (Dr. -
Open-File/Color For
Questions about Lake Manly’s age, extent, and source Michael N. Machette, Ralph E. Klinger, and Jeffrey R. Knott ABSTRACT extent to form more than a shallow n this paper, we grapple with the timing of Lake Manly, an inconstant lake. A search for traces of any ancient lake that inundated Death Valley in the Pleistocene upper lines [shorelines] around the slopes Iepoch. The pluvial lake(s) of Death Valley are known col- leading into Death Valley has failed to lectively as Lake Manly (Hooke, 1999), just as the term Lake reveal evidence that any considerable lake Bonneville is used for the recurring deep-water Pleistocene lake has ever existed there.” (Gale, 1914, p. in northern Utah. As with other closed basins in the western 401, as cited in Hunt and Mabey, 1966, U.S., Death Valley may have been occupied by a shallow to p. A69.) deep lake during marine oxygen-isotope stages II (Tioga glacia- So, almost 20 years after Russell’s inference of tion), IV (Tenaya glaciation), and/or VI (Tahoe glaciation), as a lake in Death Valley, the pot was just start- well as other times earlier in the Quaternary. Geomorphic ing to simmer. C arguments and uranium-series disequilibrium dating of lacus- trine tufas suggest that most prominent high-level features of RECOGNITION AND NAMING OF Lake Manly, such as shorelines, strandlines, spits, bars, and tufa LAKE MANLY H deposits, are related to marine oxygen-isotope stage VI (OIS6, In 1924, Levi Noble—who would go on to 128-180 ka), whereas other geomorphic arguments and limited have a long and distinguished career in Death radiocarbon and luminescence age determinations suggest a Valley—discovered the first evidence for a younger lake phase (OIS 2 or 4). -
UNIVERSITY of NOTRE DAME TRACK and FIELD HISTORY & RECORDS Men’S All-Americans Notes: All Finishes, If Available, Are Indicated in Parentheses
UNIVERSITY OF NOTRE DAME TRACK AND FIELD HISTORY & RECORDS Men’s All-Americans Notes: All finishes, if available, are indicated in parentheses. The distance medley relay, one-mile run (after 1965), two-mile relay, 55 meters, 60 meters, 55-meter hurdles, 60-meter hurdles and 3,000-meter run are indoor events only. All other indoor events are indicated. If no indoor indication exists, the event is outdoor. (y – yards; m – meters) 1921 Greg Rice .................Mile (4th), Two-Mile (1st) 1966 1994 Gus Desch ....................220y Low Hurdles (1st) 1941 Ed Dean .............................................Mile (3rd) Randy Kinder .................... Indoor 200m (10th) Billy Hayes ....................100y (2nd), 220y (4th) Jim Delaney ................................Shot Put (4th) Pete Farrell......880y (6th), Indoor 1,000y (4th) 1995 Johnny Murphy .......................High Jump (1st) John O’Rourke ........................High Jump (3rd) 1967 Eugene Oberst ...............................Javelin (1st) John Cowan ......................Steeplechase (11th) Chet Wynne ................120y High Hurdles (4th) 1942 Pete Farrell............................Indoor 880y (6th) Mike McWilliams .....................10,000m (14th) Allen Rossum....................................55m (7th) 1922 Frank Conforti ................................... Mile (4th) 1968 Jim Delaney ................................Shot Put (3rd) Ed Broderick ........................High Jump (t-4th) 1996 Billy Hayes ...................100y (2nd), 220y (2nd) Oliver Hunter .......................... -
Death Valley
DEATH VALLEY UNITED STATES DEPARTMENT OF THE INTERIOR NATIONAL PARK SERVICE UNITED STATES DEPARTMENT OF THE INTERIOR HAROLD L. ICKES, Secretary NATIONAL PARK SERVICE ARNO B. CAMMERER, Director DEATH VALLEY NATIONAL MONUMENT CALIFORNIA OPEN ALL YEAR UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1934 CONTENTS PAGE HISTORICAL INTEREST i COLORFUL SCENERY 4 GEOLOGICAL STORY 8 FOSSILS INDICATE MARINE LIFE 8 How THE VALLEY WAS FORMED 8 ANIMAL AND PLANT LIFE 14 DEATH VALLEY SCOTTY'S CASTLE 16 ACCOMMODATIONS 18 PUBLIC CAMP GROUNDS 20 How TO REACH DEATH VALLEY 20 RULES AND REGULATIONS 27 DEATH VALLEY NATIONAL MONUMENT EATH VALLEY, celebrated in history for its tragic episode in the D California gold-rush drama of '49 and famed throughout the scien tific world as a region of weird natural wonders, became a national monument on February 11, 1933, by Presidential proclamation. The 2,500 square miles included in the monument embrace Death Val ley itself and parts of the rough-hewn mountains that rise abruptly on all sides to guard its colorful desolation. The Amargosa River provides the only natural entrance. To the west towers the Panamint Range and to the east the Amargosas, with the Last Chance Range pinching the north and the Avawatz Mountains blocking the south. Death Valley National Monument lies in the southeastern corner of Inyo County and borders the California-Nevada boundary line. It forms the northern point of the great Mojave Desert region. Approximately 400 square miles of the floor of the valley lie below sea level, and Bad Water, 276 feet below mean tide, is the lowest point in the United States. -
Distribution of Amargosa River Pupfish (Cyprinodon Nevadensis Amargosae) in Death Valley National Park, CA
California Fish and Game 103(3): 91-95; 2017 Distribution of Amargosa River pupfish (Cyprinodon nevadensis amargosae) in Death Valley National Park, CA KRISTEN G. HUMPHREY, JAMIE B. LEAVITT, WESLEY J. GOLDSMITH, BRIAN R. KESNER, AND PAUL C. MARSH* Native Fish Lab at Marsh & Associates, LLC, 5016 South Ash Avenue, Suite 108, Tempe, AZ 85282, USA (KGH, JBL, WJG, BRK, PCM). *correspondent: [email protected] Key words: Amargosa River pupfish, Death Valley National Park, distribution, endangered species, monitoring, intermittent streams, range ________________________________________________________________________ Amargosa River pupfish (Cyprinodon nevadensis amargosae), is one of six rec- ognized subspecies of Amargosa pupfish (Miller 1948) and survives in waters embedded in a uniquely harsh environment, the arid and hot Mojave Desert (Jaeger 1957). All are endemic to the Amargosa River basin of southern California and Nevada (Moyle 2002). Differing from other spring-dwelling subspecies of Amargosa pupfish (Cyprinodon ne- vadensis), Amargosa River pupfish is riverine and the most widely distributed, the extent of which has been underrepresented prior to this study (Moyle et al. 2015). Originating on Pahute Mesa, Nye County, Nevada, the Amargosa River flows intermittently, often under- ground, south past the towns of Beatty, Shoshone, and Tecopa and through the Amargosa River Canyon before turning north into Death Valley National Park and terminating at Badwater Basin (Figure 1). Amargosa River pupfish is data deficient with a distribution range that is largely unknown. The species has been documented in Tecopa Bore near Tecopa, Inyo County, CA (Naiman 1976) and in the Amargosa River Canyon, Inyo and San Bernardino Counties, CA (Williams-Deacon et al. -
Historical Society of Southern California Collection -- Charles Puck Collection of Negatives and Photographs: Finding Aid
http://oac.cdlib.org/findaid/ark:/13030/tf2p30028s No online items Historical Society of Southern California Collection -- Charles Puck Collection of Negatives and Photographs: Finding Aid Finding aid prepared by Jennifer Watts. The Huntington Library, Art Collections, and Botanical Gardens Photo Archives 1151 Oxford Road San Marino, California 91108 Phone: (626) 405-2191 Email: [email protected] URL: http://www.huntington.org © August 1999 The Huntington Library. All rights reserved. Historical Society of Southern photCL 400 volume 2 & volume 3 1 California Collection -- Charles Puck Collection of Negatives a... Overview of the Collection Title: Historical Society of Southern California Collection -- Charles Puck Collection of Negatives and Photographs Dates (inclusive): 1864-1963 Bulk dates: 1920s-1950s Collection Number: photCL 400 volume 2 & volume 3 Creator: Puck, Charles, 1882-1968 Extent: 11,400 photographs in 42 boxes (30.29 linear feet) Repository: The Huntington Library, Art Collections, and Botanical Gardens. Photo Archives 1151 Oxford Road San Marino, California 91108 Phone: (626) 405-2191 Email: [email protected] URL: http://www.huntington.org Abstract: The Puck Collection consists of more than 11,000 photographs and negatives both taken and collected by Los Angeles resident and local history enthusiast Charles Puck (1882-1968), which he donated to the Historical Society of Southern California over more than twenty years in the mid-20th century. The photographs date from 1864 to 1963 (bulk 1920s-1950s) and depict buildings, monuments, civic happenings, modes of transportation, flora and fauna, and anything else that captured his particular interests. Puck compiled several scrapbooks on topics such as adobes and buildings of Los Angeles, illustrating them with his photographs and annotating them with historical anecdotes and personal recollections. -
Snowshoeing Skills Book Updated August 2012
Snowshoeing Skills Book Updated August 2012 Coaching Principles STEPS IN TEACHING A DRILL 1. Introduce 2. Demonstrate 3. Explain 4. Organize 5. Execute 6. Correct 7. Practice GENERAL PRINCIPLES Drills should relate specifically to what you are teaching. Athletes should be made aware of how drills relate to the sport. Drills should only be a part of your practice. Drills should be introduced at a slow pace and then gradually increased Drills should be accommodated for fitness, age and abilities. Drills should move from simple to complex. First perform drills that will help keep the interest of athletes. Drills should relate to the system of play that the athletes will use. Perform a variety of drills to prevent monotony. As fatigue sets in, technique deteriorates so provide frequent rest periods. EXECUTION PRINCIPLES Review the drill procedure before practice so you know how it works. When introducing a new drill, walk a group of athletes through it so others can see how it is performed. Avoid talking too much, get the athletes performing, they will learn by doing. When errors occur, the drill should be stopped momentarily to correct errors. Praise those athletes doing the drill well and encourage those having difficulty. If equipment is necessary, ensure it is set up before so that progression from one drill to the next can progress smoothly. Snowshoe Warm Up The purpose of a snowshoe warm up is really to get the legs warm up and to increase the distance of the stride. Follow these stretches with approximately 5-10 min of stretching. Ideas: Begin with a quick paced walk for one lap.