
■ MUNDY PARK CAFE 특별기획 2017-2
Artist Point(Table Mountain,Mt.Baker & Mt.Shuksan 전망대)around 눈산행
http://blog.daum.net/mundy-park/5249
http://cafe.daum.net/mundypark1/F2lJ/150
■ MUNDY PARK CAFE 특별기획 2018
■ Artist Point(Table Mountain) around 눈 산행
'MUNDY PARK CAFE 특별 기획‘은 매년 1월1일 새해맞이 엘핀레이크 시산제 산행에 이어 사진 촬영을 겸한 걷기를 비롯하여 5월 8일(화요일) ’Artist Point(Table Mtn, Mt.Baker & Mt.Shuksan 전망대)around산행‘을 실시합니다.
사진 촬영을 겸한 Snowshoes 산행을 시행 하고자 하오니 관심 있는 분들의 많은 동참 바랍니다.
4월 Ski season이 끝나고 5월 중순을 지나 눈이 녹기 시작하면 지금의 설경은 망가지고 더 이상 순백의 눈 풍경은 볼 수가 없어지게 됩니다.
사진 촬영을 겸한 Mt.Baker 주변의 설산 풍경과 아우러진 순백색의 눈 산행을 할 수 있는 마지막 기회입니다.
* 산행팀에 합류하면 안전상 개인행동은 일체 허용하지 않습니다.
1. 일자 : 2018년 5월 8일(화요일)
* 우천(雨天)시 일정 변경은 밴조선 커뮤니티>밴조선 카페> '아웃도어'에 수정 공지 예정.
2. 목적지 : Artist Point(Table Mtn, Mt.Baker & Mt.Shuksan 전망대)around
3. 산행예정시간 : 4시간~5시간 예상(스키장 정비고 주차장 ⇀ Austin Pass ⇀ 눈 덮인 Begley Lakes ⇀ Artist Point ⇀Table Mtn. around ⇀ Artist Ridge Trail ⇀ 스키장 정비고 주차장)
4. 집결장소 및 출발시간
☛ 1차 집결장소 및 출발시간(시간엄수) : 06:30 Surrey 공영주차장 [성김대건천주교회(10222 161St, Surrey, BC. V4A 2J8) 입구] : HWY 1 ⇀ Exit 50 으로 진출 후 100m 지점 네거리에서 직진 ⇀ 100m 전진후 160 St 에서 우회전 ⇀ 160 St South 50m 지점 삼거리에서 좌회전 ⇀ 103 Ave 100m 직진 후 왼쪽 'Park & Ride'(공용 주차장) : 합승비 $15.00(Park & Ride 에서 목적지 까지 115km)
☛ 2차 집결장소 및 출발시간 : 07:00 IGA Market 주차장 : HWY 1 Exit #92로 진출 ⇀ Sumas Way(ROUTE 11) 삼거리에서 좌회전 ⇀ USA Sumas(Mission) Border 통과 후 100m 오른쪽 : 합승비 $10.00(목적지 까지 72km)
5. 준비 사항 :
☛ PASS PORT(잔여기간 180일 이상), Citizenship, PR CARD, VISA : 출입국 및 산행안전에 대한 모든 책임은 본인에게 있습니다.
☛ 점심 및 간식 : 농수산물[육류, 채소, 과일(썰은것 포함)]은 소지할 수 없으며 특히, 가루제품(인삼, 누룩, 미숫가루등)은 마약으로 오인될 수 있으므로 소지를 삼가기 바랍니다.
필요한 식음료 수는 국경 통과후 IGA Markt에서 구입할 수 있습니다
☛ 필수품 : Snowshoes(스노슈즈), Trekking poles(쌍지팡이/Ski poles), Gaiters((게이터)/Spats(스패츠)/leggings(레깅스)/각반(脚絆)), Sunglasses(썬 글라스/고글), 썬 크림, 비옷, 방한복, Camera
* Snowshoes 없이는 본인의 산행이 거의 불가능하거나 전체 진행에 지장을 초래할 수가 있습니다.
☛ 참가비 : 없음
☛ 아침식사 : 산행당일 아침식사는 든든하게 하고 나올 것
☛ 산행전날 : 먼저 배낭을 꾸려놓고 일찍 취침하여 충분한 수면을 취할 것
☛ 개인안전 : 참가자 개인의 출입국문제와 산행안전은 어떠한 경우라도 그 책임이 본인에게 있음을 인지하고 개인의 문제(안전사고외) 발생 시 공동안전으로 연결되어 전체를 위험에 빠뜨리게 할 수도 있다는 사실을 꼭 명심할 것!!!
6. 산행 확인 :
안내 : 德山(604-619-8368)
http://cafe.daum.net/mundypark1
■ 2018 MUNDY PARK CAFE 특별기획
[2018-01] 1월 1일(MON) : Elfin Lakes(Squamish, BC) 새해맞이 시산제 산행
*http://cafe.daum.net/mundypark1/F2lJ/150
*http://cafe.daum.net/mundypark1/F8HK/144
*http://cafe.daum.net/mundypark1/F2lJ/160
■ Photo & Hiking 일정 확인 및 모임
[사진 촬영 및 산행]을 일기(日氣)에 따라 수시로 실시합니다
[사진, 여행, 산행]에 관심이 있는 많은 분들의 동참을 기대합니다
☞ 그룹단위 신청을 환영합니다
☞ 일정과 장소는 상황에 따라 변동 될 수도 있습니다
☞ 행사에 합류하면 공동안전(共同安全)을 위하여 개인행동을 일절 금합니다
■ 모임 안내 : 德山(604-619-8368)
http://cafe.daum.net/mundypark1
■ 生活 사진
'생활 寫眞은 일상의 사소한 발견'입니다
삼라만상(森羅萬象)은 곧 사진의 훌륭한 소재라고 생각합니다
늘 가지고 다니는 휴대전화나 손안에 쏙 들어가는 똑따기 사진기만으로도 누구나 크게 공감하고 많이 동감하는 이야기를 만들 수가 있을 것이라 믿습니다
더없는 사랑과 꾸밈없는 정성으로 人時空을 담아내어 소중한 추억으로 오래토록 간직하게 되기를 희망합니다
'사진은 빛의 예술이자 역사의 기록이다'
생활사진에 대하여 이렇게 거창한 말까지 앞세울 필요는 전혀 없을 것 같습니다
진심과 진정을 바탕으로 있는 대로 보고 보이는 대로 찍으면 됩니다
현실에 있는 대로의 진실을 보고 보이는 대로 최선을 다해 담아내면 그것이 곧 예술이자 역사가 될 것입니다
언제 어디에서 누구와 함께 하더라도 좋을것입니다
보다 많은 사진인구의 저변 확대를 기대합니다
가족의 건강과 가정의 행복을 축원합니다
오로지 건강하세요
늘 고맙습니다
20121212(陰10.29) WED
Mundy Sung
■ 삼라만상(森羅萬象)은 곧 사진(寫眞)의 소재입니다
사진은 무엇으로 어떻게 찍든 간에 있는 대로 보고 보이는 대로 찍으면 된다고 생각합니다
이것이야말로 진정한 빛의 예술이자 진실된 역사의 기록이 아닐는지요
--------------------
■ 우울증, 전 세계 3억2천만 명 10년 사이 18% 증가 - 송고시간 | 2017/02/24 02:19
(제네바=연합뉴스) 이광철 특파원 = 전 세계 인구 4%에 해당하는 3억2천200만 명이 우울증을 앓고 있으며 노인, 여성, 청소년 등이 특히 취약한 것으로 조사됐다고 세계보건기구(WHO)가 23일(현지시간) 밝혔다
WHO는 2015년 기준으로 집계한 우울증 인구가 2005년보다 18.4% 증가했다며 인구 증가뿐 아니라 기대 수명이 늘어난 것도 원인으로 작용했다고 설명했다
우울증으로 인한 각종 부작용은 삶의 후반기에 막대한 영향을 미치고 있다
☞ [자살공화국, 하루에 40여명이 生을 포기한다] http://cafe.daum.net/mundypark1/DPKO/598
☞ [이건세 교수의 사진 잘 찍는 법 50] http://cafe.daum.net/mundypark1/CsVj/130
☞ [셀카 찍는다고 자존심이 회복돼?] https://storyfunding.daum.net/episode/4766
☞ [사진 찍기, 여행 즐거움을 향상 시킬까?] http://cafe.daum.net/kvwc/dvOn/1
☞ [할머니의 카메라] https://storyfunding.daum.net/episode/4752
☞ [멋진 노을 사진 찍는 법] http://cafe.daum.net/kvwc/dvOn/2
--------------------
최근 조사결과 캐나다인들 병원 방문 이유 1위가 우울증이라고 합니다
사진촬영이나 걷기는 우울증 예방이나 치료에도 상당한 효과가 있다고 합니다
사진을 좋아하거나 관심 있는 많은 분들의 동참을 기대하며 사진 인구의 저변확대를 소망합니다
■ 산행 안전
■ [산행 안전 수칙] 즐거운 산행을 위하여
http://cafe.daum.net/mundypark1/CP3B/175
http://cafe.daum.net/mundypark1/CP3B/41
http://www.vkhc.com/xe/HikingTip/1513
■ [동절기 안전산행 필수품]
http://cafe.daum.net/mundypark1/CP3B/174
http://cafe.daum.net/mundypark1/CP3B/40
http://www.vkhc.com/xe/HikingTip/1516
■ [겨울철 눈산행시 주의할 점]
http://cafe.daum.net/mundypark1/CP3B/173
http://cafe.daum.net/mundypark1/CP3B/39
http://www.vkhc.com/xe/HikingTip/1517
■ Mt.Baker(10,781ft/3,286m)
Mount Baker
| Mount Baker | |
|---|---|
| Kulshan | |
Mount Baker as seen from the Southeast at Boulder Creek | |
| Highest point | |
| Elevation | 10,781 ft (3,286 m) [1] |
| Prominence | 8,812 ft (2,686 m) [1] |
| Listing | |
| Coordinates | |
| Geography | |
| Location | Whatcom County, Washington, U.S. |
| Parent range | Cascade Range[3] |
| Topo map | USGS Mount Baker |
| Geology | |
| Age of rock | Less than 140,000 years[5] |
| Mountain type | Stratovolcano[4] |
| Volcanic arc | Cascade Volcanic Arc[3] |
| Last eruption | September to November 1880[6] |
| Climbing | |
| First ascent | 1868 by Edmund Coleman, John Tennant, Thomas Stratton and David Ogilvy[7][8] |
| Easiest route | snow (ice) climb |
Mount Baker (Lummi: Qwú’mə Kwəlshéːn; Nooksack: Kw’eq Smaenit or Kwelshán), also known as Koma Kulshan or simply Kulshan, is an active[9] glaciated andesitic stratovolcano [4] in the Cascade Volcanic Arc and the North Cascades of Washington in the United States. Mount Baker has the second-most thermally active crater in the Cascade Range after Mount Saint Helens.[10] About 31 miles (50 km)[11] due east of the city of Bellingham, Whatcom County, Mount Baker is the youngest volcano in the Mount Baker volcanic field.[5] While volcanism has persisted here for some 1.5 million years, the current glaciated cone is likely no more than 140,000 years old, and possibly no older than 80–90,000 years. Older volcanic edifices have mostly eroded away due to glaciation.
After Mount Rainier, Mount Baker is the most heavily glaciated of the Cascade Range volcanoes; the volume of snow and ice on Mount Baker, 0.43 cu mi (1.79 km3) is greater than that of all the other Cascades volcanoes (except Rainier) combined. It is also one of the snowiest places in the world; in 1999, Mount Baker Ski Area, located 14 km (8.7 mi) to the northeast, set the world record for recorded snowfall in a single season—1,140 in (2,900 cm).[12]
At 10,781 ft (3,286 m), it is the third-highest mountain in Washington State and the fifth-highest in the Cascade Range, if Little Tahoma Peak, a subpeak of Mount Rainier, and Shastina, a subpeak of Mount Shasta, are not counted.[4][13] Located in the Mount Baker Wilderness, it is visible from much of Greater Victoria, Nanaimo, and Greater Vancouver in British Columbia and, to the south, from Seattle (and on clear days Tacoma) in Washington.
Indigenous Peoples have known the mountain for thousands of years, but the first written record of the mountain is from Spanish explorer Gonzalo Lopez de Haro, who mapped it in 1790 as Gran Montaña del Carmelo, "Great Mount Carmel".[14] The explorer George Vancouver renamed the mountain for 3rd Lieutenant Joseph Baker of HMS Discovery, who saw it on April 30, 1792.[15]
Mount Baker was well-known to indigenous peoples of the Pacific Northwest. Indigenous names for the mountain include Koma Kulshan or Kulshan (Lummi: qwú’mə, "white sentinel", , and kwəlshé:n, "puncture wound", i.e. "crater");[16][17][18] Quck Sam-ik (Nooksack: kw’eq sámit, "white mountain");[19] Kobah (Skagit: qwúbə’, "white sentinel", and Tukullum or Nahcullum (in the language of the unidentified "Koma tribe").[20]
In 1790, Manuel Quimper of the Spanish Navy set sail from Nootka, a temporary settlement on Vancouver Island, with orders to explore the newly discovered Strait of Juan de Fuca. Accompanying Quimper was first-pilot Gonzalo Lopez de Haro, who drew detailed charts during the six-week expedition. Although Quimper's journal of the voyage does not refer to the mountain, one of Haro's manuscript charts includes a sketch of Mount Baker.[21][22] The Spanish named the snowy volcano La Gran Montana del Carmelo, as it reminded them of the white-clad monks of the Carmelite Monastery.[23]
The British explorer George Vancouver left England a year later. His mission was to survey the northwest coast of America. Vancouver and his crew reached the Pacific Northwest coast in 1792. While anchored in Dungeness Bay on the south shore of the Strait of Juan de Fuca, third lieutenant Joseph Baker made an observation of Mount Baker, which Vancouver recorded in his journal:
About this time a very high conspicuous craggy mountain ... presented itself, towering above the clouds: as low down as they allowed it to be visible it was covered with snow; and south of it, was a long ridge of very rugged snowy mountains, much less elevated, which seemed to stretch to a considerable distance ... the high distant land formed, as already observed, like detached islands, amongst which the lofty mountain, discovered in the afternoon by the third lieutenant, and in compliment to him called by me Mount Baker, rose a very conspicuous object ... apparently at a very remote distance.[22]
Six years later, the official narrative of this voyage was published, including the first printed reference to the mountain.[22] By the mid-1850s, Mount Baker was a well-known feature on the horizon to the explorers and fur traders who traveled in the Puget Sound region. Isaac I. Stevens, the first governor of Washington Territory, wrote about Mount Baker in 1853:
Mount Baker ... is one of the loftiest and most conspicuous peaks of the northern Cascade range; it is nearly as high as Mount Rainier, and like that mountain, its snow-covered pyramid has the form of a sugar-loaf. It is visible from all the water and islands ... [in Puget Sound] and from the whole southeastern part of the Gulf of Georgia, and likewise from the eastern division of the Strait of Juan de Fuca. It is for this region a natural and important landmark.[22]
Edmund Thomas Coleman, an Englishman who resided in Victoria, British Columbia, Canada and a veteran of the Alps, made the first attempt to ascend the mountain in 1866. He chose a route via the Skagit River, but was forced to turn back when local Native Americans refused him passage.[14]
Later that same year, Coleman recruited Whatcom County settlers Edward Eldridge, John Bennett and John Tennant to aid him in his second attempt to scale the mountain. After approaching via the North Fork of the Nooksack River, the party navigated through what is now known as Coleman Glacier and ascended to within several hundred feet of the summit before turning back in the face of an "overhanging cornice of ice" and threatening weather.[14] Coleman later returned to the mountain after two years. At 4:00 p.m. on August 17, 1868, Coleman, Eldridge, Tennant and two new companions (David Ogilvy and Thomas Stratton) scaled the summit via the Middle Fork Nooksack River, Marmot Ridge, Coleman Glacier, and the north margin of the Roman Wall.[14]
The present-day cone of Mount Baker is relatively young; it is perhaps less than 100,000 years old.[5] The volcano sits atop a similar older volcanic cone called Black Buttes, which was active between 500,000 and 300,000 years ago.[25] Much of Mount Baker's earlier geological record eroded away during the last ice age (which culminated 15,000–20,000 years ago), by thick ice sheets that filled the valleys and surrounded the volcano. In the last 14,000 years, the area around the mountain has been largely ice-free, but the mountain itself remains heavily covered with snow and ice.[26]
Isolated ridges of lava and hydrothermally altered rock, especially in the area of Sherman Crater, are exposed between glaciers on the upper flanks of the volcano; the lower flanks are steep and heavily vegetated. Volcanic rocks of Mount Baker and Black Buttes rest on a foundation of non-volcanic rocks.[5]
Deposits recording the last 14,000 years at Mount Baker indicate that Mount Baker has not had highly explosive eruptions like those of other volcanoes in the Cascade Volcanic Arc, such as Mount St. Helens, Mount Meager or Glacier Peak, nor has it erupted frequently. During this period, four episodes of magmatic eruptive activity have been recently recognized.[27][28]
Magmatic eruptions have produced tephra, pyroclastic flows, and lava flows from summit vents and the Schriebers Meadow cinder cone. The most destructive and most frequent events at Mount Baker have been lahars or debris flows and debris avalanches; many, if not most, of these were not related to magmatic eruptions but may have been induced by magma intrusion, steam eruptions, earthquakes, gravitational instability, or possibly even heavy rainfall.[26][27][29]
Research beginning in the late 1990s shows that Mount Baker is the youngest of several volcanic centers in the area and one of the youngest volcanoes in the Cascade Range.[5][29] The Pliocene Hannegan caldera is preserved 16 miles (25 km) northeast of Mount Baker [30][31] Volcanic activity in the Mount Baker volcanic field began more than one million years ago, but many of the earliest lava and tephra deposits have been removed by glacial erosion. The pale-colored rocks northeast of the modern volcano mark the site of the ancient (1.15 million years old) Kulshan caldera that collapsed after an enormous ash eruption one million years ago. Subsequently, eruptions in the Mount Baker area have produced cones and lava flows of andesite, the rock that constitutes much of other Cascade Range volcanoes such as Rainier, Adams, and Hood. From about 900,000 years ago to the present, numerous andesitic volcanic centers in the area have come and disappeared through glacial erosion. The largest of these cones is the Black Buttes edifice, active between 500,000 and 300,000 years ago and formerly bigger than today's Mount Baker.[9][32]
Mount Baker was built from stacks of lava and volcanic breccia prior to the end of the last glacial period, which ended about 15,000 years ago. There are two craters on the mountain. Ice-filled Carmelo Crater is under the summit ice dome.[5] This crater is the source for the last cone-building eruptions[33][34] The highest point of Mount Baker, Grant Peak, is on the exposed southeast rim of Carmelo Crater, which is a small pile of andesitic scoria lying on top of a stack of lava flows just below. Carmelo Crater is deeply dissected on its south side by the younger Sherman Crater. This crater is south of the summit, and its ice-covered floor is 1,000 ft (300 m) below the summit ice dome. This crater is the site of all Holocene eruptive activity.[27] Hundreds of fumaroles vent gases, primarily H
2O, CO
2, and H
2S.[29][35]
Lava flows from the summit vent erupted between 30,000 and 10,000 years ago and, during the final stages of edifice construction, blocky pyroclastic flows entered the volcano's southeastern drainages.[34] An eruption from Sherman Crater 6,600 years ago erupted a blanket of ash that extended more than 40 mi (64 km) to the east.[36] Today, sulfurous gases reach the surface via two fumarole pathways: Dorr Fumarole, northeast of the summit; and Sherman Crater, south of the summit. Both are sites of hydrothermal alteration, converting lavas to weak, white-to-yellow clays; sulfur is a common mineral around these fumaroles. At Sherman Crater, collapses of this weakened rock generated lahars in the 1840s.[27][37]
Approximately 6,600 years ago, a series of discrete events culminated in the largest tephra-producing eruption in post-glacial time at Mount Baker. This is the last episode of undoubted magmatic activity preserved in the geologic record.[5] First, the largest collapse in the history of the volcano occurred from the Roman Wall and transformed into a lahar that was over 300 feet (91 m) deep in the upper reaches of the Middle Fork of the Nooksack River. It was at least 25 ft (7.6 m) deep 30 mi (48 km) downstream from the volcano.[27] At that time the Nooksack River is believed to have drained north into the Fraser River; it is therefore unlikely that this lahar reached Bellingham Bay. Next, a small hydrovolcanic eruption occurred at Sherman Crater, triggering a second collapse of the flank just east of the Roman Wall. That collapse also became a lahar that mainly followed the course of the first lahar for at least 20 mi (32 km), and also spilled into tributaries of the Baker River. Finally, an eruption cloud deposited ash as far as 40 mi (64 km) downwind to the northeast and east.[36]
Several eruptions occurred from Sherman Crater during the 19th century;[38] they were witnessed from the Bellingham area.[39] A possible eruption was seen in June 1792 during the Spanish expedition of Dionisio Alcalá Galiano and Cayetano Valdés. Their report read, in part:
During the night [while anchored in Bellingham Bay] we constantly saw light to the south and east of the mountain of Carmelo [Baker] and even at times some bursts of flame, signs which left no doubt that there are volcanoes with strong eruptions in those mountains.[40]
In 1843, explorers reported a widespread layer of newly fallen rock fragments "like a snowfall" and that the forest was "on fire for miles around". It is highly unlikely that these fires were caused by ashfall, however, as charred material is not found with deposits of this fine-grained volcanic ash, which was almost certainly cooled in the atmosphere before falling. Rivers south of the volcano were reportedly clogged with ash, and Native Americans reported that many salmon perished. Reports of flooding on the Skagit River from the eruption are, however, probably greatly exaggerated.[41] A short time later, two collapses of the east side of Sherman Crater produced two lahars, the first and larger of which flowed into the natural Baker Lake, increasing its level by at least 10 feet (3.0 m). The location of the 19th-century lake is now covered by waters of the modern dam-impounded Baker Lake. Similar but lower level hydrovolcanic activity at Sherman Crater continued intermittently for several decades afterward.[32][39] On 26 November 1860, passengers who were traveling by steamer from New Westminster to Victoria reported that Mount Baker was "puffing out large volumes of smoke, which upon breaking, rolled down the snow-covered sides of the mountain, forming a pleasing effect of light and shade."[42] In 1891, about 15 km3 (3.6 cu mi) of rock fell producing a lahar that traveled more than 6 mi (9.7 km) and covered 1 sq mi (2.6 km2).[43]
Activity in the 20th century decreased from the 19th century. Numerous small debris avalanches fell from Sherman Peak and descended the Boulder Glacier; a large one occurred on July 27, 2007.[44][45]
In early March 1975, a dramatic increase in fumarolic activity and snow melt in the Sherman Crater area raised concern that an eruption might be imminent.[26] Heat flow increased more than tenfold.[9][32] Additional monitoring equipment was installed and several geophysical surveys were conducted to try to detect the movement of magma.[26] The increased thermal activity prompted public officials and Puget Power to temporarily close public access to the popular Baker Lake recreation area and to lower the reservoir's water level by 33 feet (10 m). If those actions had not been taken, significant avalanches of debris from the Sherman Crater area could have swept directly into the reservoir, triggering a disastrous wave that could have caused human fatalities and damage to the reservoir.[39][46] Other than the increased heat flow, few anomalies were recorded during the geophysical surveys, nor were any other precursory activities observed that would indicate that magma was moving up into the volcano.[26] Several small lahars formed from material ejected onto the surrounding glaciers and acidic water was discharged into Baker Lake for many months.[9][32]
Activity gradually declined over the next two years but stabilized at a higher level than before 1975.[9][32] The increased level of fumarolic activity has continued at Mount Baker since 1975, but no other changes suggest that magma movement is involved.[26]
A considerable amount of research has been done at Mount Baker over the past decade, and it is now among the most-studied of the Cascade volcanoes. Recent and ongoing projects include gravimetric and GPS-based geodetic monitoring, fumarole gas sampling, tephra distribution mapping, new interpretations of the Schriebers Meadow lava flow, and hazards analyses. Mapping of Carmelo and Sherman craters, and interpretations of the eruptive history, continues, as well. The Mount Baker Volcano Research Center[29] maintains an online archive of abstracts of this work, and an extensive references list, as well as photos.
There are ten main glaciers on the mountain. The Coleman Glacier is the largest; it has a surface area of 5.2 square kilometers (1,280 acres).[47] The other large glaciers—which have areas greater than 2.5 km2 (620 acres)—are Roosevelt Glacier, Mazama Glacier, Park Glacier, Boulder Glacier, Easton Glacier and Deming Glacier.[47][48] All retreated during the first half of the century, advanced from 1950–1975 and have been retreating increasingly rapidly since 1980.[49][50][51][52]
Mount Baker is drained on the north by streams that flow into the North Fork Nooksack River, on the west by the Middle Fork Nooksack River, and on the southeast and east by tributaries of the Baker River.[53] Lake Shannon and Baker Lake are the largest nearby bodies of water, formed by two dams on the Baker River.
Two ammunition ships of the United States Navy (traditionally named for volcanoes) have been named after the mountain. The first was USS Mount Baker (AE-4), which was commissioned from 1941 to 1947 and from 1951 to 1969.[54] In 1972, the Navy commissioned USS Mount Baker (AE-34). It was decommissioned in 1996 and placed in service with the Military Sealift Command as USNS Mount Baker (T-AE-34).[55] She was scrapped in 2012.
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| Mount Shuksan | |
|---|---|
| Highest point | |
| Elevation | 9,131 ft (2,783 m) NGVD 29[1] |
| Prominence | 4,411 ft (1,344 m) [1] |
| Coordinates | |
| Geography | |
| Location | Whatcom County, Washington, U.S. |
| Parent range | Cascades |
| Topo map | USGS Mount Shuksan |
| Geology | |
| Age of rock | Cretaceous |
| Mountain type | Metamorphic schist |
| Climbing | |
| First ascent | September 7, 1906 by Asahel Curtis and party |
| Easiest route | rock/ice climb, class 3[1] |
Mount Shuksan is a glaciated massif[3] in the North Cascades National Park. Shuksan rises in Whatcom County, Washington immediately to the east of Mount Baker, and 11.6 miles (18.7 km) south of the Canada–US border. The mountain's name Shuksan is derived from the Lummi word [šéqsən], said to mean "high peak".[4] The highest point on the mountain is a three sided peak known as Summit Pyramid.[5]
The mountain is composed of Shuksan greenschist, oceanic basalt that was metamorphosed when the Easton terrane collided with the west coast of North America, approximately 120 million years ago.[6] The mountain is an eroded remnant of a thrust plate formed by the Easton collision.[3]
Mount Shuksan may be one of the most photographed mountains in the Cascade Range.[7] Photographs with its reflection in Picture Lake near Mount Baker Ski Area are particularly common. The Mount Baker Highway, State Route 542, is kept open during the winter to support the ski area; in late summer, the road to Artist Point allows visitors to travel a few miles higher for a closer view of the peak.
Sulphide Creek Falls, one of the tallest waterfalls in North America, plunges off the southeastern flank of Mount Shuksan. There are four other tall waterfalls that spill off Mount Shuksan and neighboring Jagged Ridge and Seahpo Peak, mostly sourced from small snowfields and glaciers.
The traditional name of Mount Shuksan in the Nooksack language is Shéqsan ("high foot") or Ch’ésqen ("golden eagle").[8]
The first ascent of Mount Shuksan is usually attributed to Asahel Curtis and W. Montelius Price on September 7, 1906. However, in a letter to the editor of the Mazamas club journal, C. E. Rusk attributed the first ascent to Joseph Morowits in 1897 and also stated that he would have attempted it in 1903 if he had not been sure that it had already been climbed.[9]
| Wikimedia Commons has media related to Mount Shuksan. |
■ Table Mountain
■ Artist Point : Mount Baker-Snoqualmie National Forest,
Deming,(Bellingham, Whatcom County) Washington 98244, U.S(wsdot.wa.gov/1-360-856-5700)
http://www.wsdot.wa.gov/Northwest/Baker/ArtistPoint

Artist Point
3:20 p.m. April 18, 2017
Status: CLOSED
Artist Point is located at the very end of Mount Baker Highway, State Route 542 and boasts 360-degree views of Mount Shuksan and Mount Baker, as well as access to a variety of trails.
The road to Artist Point, 2.7 miles long (milepost 54.55 to 57.26) and more than 5,000 feet above sea level, is typically buried under snow and closed October through June.
The road to Artist Point typically opens in July and remains open until the first substantial snowfall of the year, which usually comes in late September or early October.
Contacts
Trail and hiking information
Mt. Baker Ranger District Office
360-856-5700 ext 515
810 State Route 20
Sedro-Woolley, WA 98284
Glacier Public Service Center
360-599-2714
Glacier, WA 98244
Road-related questions
WSDOT communications
Andrea Petrich
360-757-5963 (No trail or hiking information available at this number.)
■ Table Mountain
■ Table Mountain
■ Table Mountain
■ Mt.Shuksan(9,131ft/2,783m)
■ Mt.Shuksan(9,131ft/2,783m)
■ Mt.Baker(10,781ft/3,286m)
■ Table Mountain
■ Mt.Baker(10,781ft/3,286m)
■ Mt.Baker(10,781ft/3,286m)
■ Table Mountain
■ Table Mountain
■ Mt.Shuksan(9,131ft/2,783m)
■ Mt.Shuksan(9,131ft/2,783m)
■ Table Mountain
■ Table Mountain
■ Table Mountain
■ 生活 사진
생활 寫眞은 일상의 사소한 발견입니다
삼라만상(森羅萬象)은 곧 사진의 훌륭한 소재라고 생각합니다.
늘 가지고 다니는 휴대전화나 손안에 쏙 들어가는 똑따기 사진기만으로도 누구나 크게 공감하고 많이 동감하는 이야기를 만들 수가 있을 것이라 믿습니다.
더없는 사랑과 꾸밈없는 정성으로 人時空을 담아내어 소중한 추억으로 오래토록 간직하게 되기를 희망합니다.
'사진은 빛의 예술이자 역사의 기록이다'
생활사진에 대하여 이렇게 거창한 말까지 앞세울 필요는 전혀 없을 것 같습니다.
진실과 진심으로 있는 대로 보고 진정과 최선을 다하여 보이는 대로 담아내면 그것이 곧 예술이자 역사가 될 것입니다
보다 많은 사진인구의 저변 확대를 기대합니다.
가족의 건강과 가정의 행복을 축원합니다.
오로지 건강하세요.
늘 고맙습니다.
20121212(陰1029) WED
Mundy Sung
■ MUNDY PARK CAFE 특별기획 2017
[2017-01] 1월 2일(MON) : Elfin Lakes(Squamish, BC) 새해맞이 시산제 산행
[2017-02] 5월 9일(TUE) : Artist Point(Table Mountain,Mount Baker & Mount Shuksan 전망대)around(WA.USA) 눈산행
■ Photo & Hiking 일정 확인 및 모임 안내
[사진 촬영 및 산행]을 일기(日氣)에 따라 수시로 실시합니다.
[사진, 여행, 산행]에 관심이 있는 많은 분들의 동참을 기대합니다.
☞ 일정과 장소는 상황에 따라 변동 될 수도 있습니다.
☞ 행사에 합류하면 공동안전(共同安全)을 위하여 개인행동을 일절 금합니다.
http://cafe.daum.net/kvwc/E3Wn/3
http://blog.daum.net/mundy-park/4370
http://cafe.daum.net/mundypark1/F2lJ/1
☞ 주관 : [MUNDY PARK CAFE]
☞ 안내 : 604-619-8368
http://cafe.daum.net/mundypark1
http://blog.daum.net/mundy-park
☞ 밴조선 커뮤니티 아웃도어
-----------------------------------
■ 삼라만상(森羅萬象)은 곧 사진(寫眞)의 소재다
사진은 무엇으로 어떻게 찍든 간에 있는 대로 보고 보이는 대로 찍으면 된다.
이것이야말로 진정한 빛의 예술이자 진실한 역사의 기록인 것이다
우울증, 전세계 3억2천만명 10년새 18% 증가 - 송고시간 | 2017/02/24 02:19
(제네바=연합뉴스) 이광철 특파원 = 전 세계 인구 4%에 해당하는 3억2천200만명이 우울증을 앓고 있으며 노인, 여성, 청소년 등이 특히 취약한 것으로 조사됐다고 세계보건기구(WHO)가 23일(현지시간) 밝혔다.
WHO는 2015년 기준으로 집계한 우울증 인구가 2005년보다 18.4% 증가했다며 인구 증가뿐 아니라 기대 수명이 늘어난 것도 원인으로 작용했다고 설명했다.
우울증으로 인한 각종 부작용은 삶의 후반기에 막대한 영향을 미치고 있다.
최근 조사결과 캐나다인들 병원 방문 이유 1위가 우울증이라고 합니다.
사진촬영이나 걷기는 우울증 예방이나 치료에도 상당한 효과가 있다고 합니다.
사진을 좋아하거나 관심 있는 많은 분들의 동참을 기대하며 사진 인구의 저변확대를 소망합니다.
☞ [사진 찍기, 여행 즐거움을 향상 시킬까?] http://cafe.daum.net/kvwc/dvOn/1
☞ [이건세 교수의 사진 잘 찍는 법 50] http://cafe.daum.net/mundypark1/CsVj/130
☞ [셀카 찍는다고 자존심이 회복돼?] https://storyfunding.daum.net/episode/4766
☞ [멋진 노을 사진 찍는 법] http://cafe.daum.net/kvwc/dvOn/2
☞ [할머니의 카메라] https://storyfunding.daum.net/episode/4752
■ Table Mountain
■ Table Mountain
■ Table Mountain
■ Table Mountain
■ Ptarmigan Ridge(타미간 릿지) Trail
■ Artist Point 에서 출발 하여 Mt.Baker(10,781ft/3,286m) 전망대 가는길
■ Living Information
