Depression Post-Mortem
View allAll Photos Tagged detachment.
Detachment is not giving up the things in this world, but accepting the fact and to be continuously aware that nothing is permanent.
~ Aditya Ajmera
I took this yesterday on a photo outing at Whytecliff Park in West Vancouver with two Flickr friends.
I will try to catch up with all of you today...
Iceberg formed by the detachment of the Perito Moreno glacier. Without an object to compare with and standing at a distance, it is very difficult to determine whether the iceberg is large or small. In fact, it seemed tiny compared to the wall of the glacier.
Sailing close to the glacier, the ship in the picture - which was a slightly smaller than ours - passed in front of this 'tiny' iceberg.
📍 Shot taken at the North side of the Perito Moreno Glacier, Los Glaciares National Park, El Calafate, Lago Argentino, Santa Cruz, Argentina
- - - detachment from civilian life felt by many WWI soldiers upon returning home from the front.
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camera: Holga 120
film: Holga 400
long exposure at 11pm: 21 seconds
The Boat is approaching the Boat Jetty.. From Were I Embarked To Take the Boat Ride,,.. I Felt That Sence Of Detachment.. From The Worldly Bonds.. and Jelled With The Beautiful Nature..
From The Silence I Felt.. It Was The Same Sence Of Feel To My Co Passangers Too... .
LOCATION : ERNAKULAM BOAT JETTY. Cochin City. Kerala State. INDIA
On the left side of the photo a bright red hogbeck made up of red shales, siltstones and sandstones that Geologists describe as the Chugwater Formation lies along the Chief Joseph Highway (Wyoming Route 296). These red beds were deposisted between 251.9 to 201.3 million of years ago during the Triassic Era. The ridge is capped by white gypsum beds that formed during the early Jurrasic (Gypsum Springs Formation), and greenish sandstone and shales from the middle Jurrasic (Sundance Formation), This view looks down from the road as it climbs Dead Indian Hill into the Bighorn Basin. In the center right, Heart Mountain can be seen.The top of Heart Mountain, is composed of Paleozoic limestone. These older rocks lie on top of the younger Tertiary and Cretaceous strata. In Geology when older rocks are out of place stratagraphically there is a tectonic or structural reason. In this case, the Paleozoic rocks, mostly Mississippian Madison Limestone, slid into place on top of the younger rock during a very large landslide event related to uplift and volcanic eruptions during the development of the Eocene Absaroka Volcanic Complex to the west. Geologist still debate the mechanisms that allow a low angle landslide to move over such a large surface area. Historically, geologists have referred to the surface between the older and younger rocks (the landslide base) as the Heart Mountain Detachment.
In this view of the north end of Sugarloaf Mountain, dipping beds of Ordovician Bighorn Dolomite rests on flat-lying Cambrian Pilgram Limestone and Park Shale. The surface between the dipping and flat lying beds is the Heart Mountain Detachment fault. The mountain can be seen from the Chief Joseph Highway (WY 296) in Shoshone National Forest northwest of Cody, Wyoming.
In this view of the north end of Sugarloaf Mountain, dipping beds of Ordovician Bighorn Dolomite rests on flat-lying Cambrian Pilgram Limestone and Park Shale. The surface betwen the two is the Heart Mountain Detachment fault. the mountain can be seen from the Chief Joseph Highway (WY 296) in Shoshone National Forest northwest of Cody, Wyoming.
Heart Mountain rises above the Chapman Bench. The hills-just above the bench are made up of Cretaceous and Tertiary shales and sandstone. The top of Heart Mountain, on the other hand, is composed of much older Paleozoic limestone. These older rocks lie on top of the younger Tertiary and rocks Cretaceous sediments. In Geology when older rocks are out of place stratagraphically there is a tectonic or structural reason. In this case, the Paleozoic rocks, mostly Mississippian Madison Limestone, slid into place on top of the younger rock during a very large landslide event related to uplift and volcanic eruptions during the development of the Eocene Absaroka Volcanic Complex to the west. Geologist still debate the mechanisms that allow a low angle landslide to move over such a large surface area. Historically, geologists have referred to the surface between the older and younger rocks (the landslide base) as the Heart Mountain Thrust or Detachment.
The road in the foreground leads up to a stock pond located where the trees stand in the photo. Heart Mountain rises above the stock pond on the horizon on the left f the photo. On the bare hill just behind the trees, the strata dip toward the center of the hill The beds on the left dip to the right and those on the right dip to the left. This is a surface expression of the syncline that runs to the west of the Shoshone anticline. The hills are made up of Cretaceous shales and sandstone. Heart Mountain, on the other hand, is composed of much older Paleozoic limestone. These older rocks lie on younger Tertiary rocks that stratigraphically overlie the Cretaceous sediments. The Paleozoic rocks, mostly Mississippian Madison Limestone, slid into place on top of the younger rock during a very large landslide event related to the development and eruptions of the Eocene Absaroka Volcanic Complex to the west. Geologist still debate the mechanisms that allow a low angle landslide to move over such a large surface area. Historically, geologists have referred to the surface between the older and younger rocks (the landslide base) as the Heart Mountain Thrust or Detachment.
April 25 2023; New York JFK. Arriving from IAD to pick up Russian Foreign Minister Sergey Lavrov after the UN Security Council meeting yesterday in New York.
For detachment is not a withdrawal from love, but an expansion of of love beyond desire. Desire is entangled in time, nostalgic for the past, preoccupied with the future. Love expanding beyond desire is “liberation from the future as well as the past.” What remains is the now “where past and future are gathered,” the “still point.”
-Brother David Steindl-Rast, A Listening Heart-The Spirituality of Sacred Sensuousness
Is not about you and me. It is not about selfish asceticism either. It is about being. Being part of and responding to, life. Master Eckhart was a medieval philosopher-theologian, and it is quite illuminating what synonymous terms he used in order to describe "detachment" (abgescheidenheit and gelazenheit in the vernacular): un-forming (entbilden), un-becoming (entwerden), peeling off (abeschelen), alienate (entvremden), loosen (abeloesen) and becoming free (vri, ledic), true (luter) and naked (bloz). Letting go is hard work.
Abandoned farmhouse on Scenic Bluff Road along with its detached garage near Savanna,IL. The garage was full of belongings emptied from the house,which despite being made of brick,is showing severe decay inside from a leaky roof...
and yes,that's my car reflected in the dresser mirror in the garage! LOL
Canadian tanker on detachment to Palmer, AK for the summer season. It was in action later the same day against a fire on the Kenai peninsula. With the other remaining Conair 580s, C-FKFA was withdrawn from service at the end of the 2022 fire season but it is intended to keep it airworthy for airshow work.
I previously saw this aircraft when it was in temporary storage at Tucson AZ in 1987. Note that for its firefighting role the radar radome has been replaced with the original short nose for enhanced pilot visibility.
Shot wide-open, contre-jour. "immovable detachment brings man into utmost sameness with God" (Unbewegelichiu abgescheidenheit bringet den menschen in die groeste glicheit mit gote; Master Eckhart, On Detachment).
Sheep Mountain, located west of Cody Wyoming, is capped with Paleozoic Carbonates. They overlie a normal sequence of Upper Cretaceous shales and interbedded sandstones. The contact between the Paleozoic rocks and the Cretaceous sediments is a surface called the Heart Mountain Detachment. The Paleozoic rocks are part of a large landslide block that slid over 28 miles around 49 million years ago. The landslide broke away from the mountains to the west and moved catastrophically down a 2 degree slope. The landslide broke apart and remnants of the Heart Mountain Detachment are found scattered over an area thought to be between 1,300 and 1,900 square miles. Sheep Mountain is one of these remnant blocks. The namesake for the Detachment is another block, Heart Mountain, that is separate and located north of Cody. Over the years, unraveling how this massive landslide occurred and transported such a large volume of rock over a great distance has been the source of debate and controversy among geologists. The Heart Mountain Detachment has been interpreted as a large scale collapse feature from the flank of an active volcanic center. Though most geologists agree with this interpretation, the mechanism that allowed the emplacement of such a large block across a nearly flat surface is a topic of much discussion and is not entirely understood. Several mechanism have been proposed. One of the most recent ideas centers around the release of gas, probably CO2, along the landslide detachment surface that allowed it to move like a hovercraft across the flat surface. Since there still are outstanding scientific questions, geologists will continue to study and debate the origins and emplacement of this landslide.
Tu-214SUS (airborne communication center) with tail number of RA-64524 of Rossiya special aircraft division (SAD) of Department for Presidental Affairs of RF taxiing for take-off at Vnukovo airport
Dunnet bay, Scotland.
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During the Balkan Wars, the previously Ottoman city of Scutari fell 1913 to Serbia and Montenegro after a seven-month siege. However, an international conference in London awarded the city to the young state of Albania. An international naval blockade involving the German cruiser Breslau forced the withdrawal of troops from Scutari. An international corps of British, German, French, Italian and Austro-Hungarian contingents was formed as military security. The German contribution consisted of a company-sized naval infantry detachment of 120 volunteers.