Prayers and Meditations by the Mother


Akakura: 13 July 1917  

 

One day I wrote: “My heart has fallen asleep down to the very depths of my being.”

 

Merely asleep? I cannot believe it. I think it is completely hushed, perhaps for ever. From sleep one awakes, from this quietness there is no falling back. And since that day I have not observed any relapse. In place of something very intensely concentrated which for a long while was intermittently tumultuous, has come an immensity so vast and calm and untroubled, filling my being; or rather my being has melted into that; for how could that which is limitless be contained in a form?

 

And these great mountains with their serene contours which I see from my window, range after majestic range up to the very horizon, are in perfect harmony with the rhythm of this being, filled with an infinite peace. Lord, couldst Thou have taken possession of Thy kingdom? Or rather of this part of the kingdom, for the body is still obscure and ignorant, slow to respond, without plasticity. Will it be purified one day like the rest? And will Thy victory then be total? It matters little. This instrument is what Thou wantest it to be and its bliss is unalloyed.  


The following are from Internet postings


Akakura Mountain Shrine

Immortal Wishes is based on Dr Ellen Schattschneider's field research at Akakura Mountain Shrine (Akakurayama Jinja) on the lower slope of Akakura Mountain, at the southern end of the Tusgaru Plain, in Aomori Prefecture, northern Tohoku, Japan.

Akakura Mountain Gorge

Akakura Mountain Gorge, looms large in the iconography and ritual practice of the shrine. It is characterized by many dramatic volcanic and geological features, and is compared by many worshippers to a woman's genitalia, "the thing of a woman". Through it runs Akakura river, the source of the life-giving water of the gods. The gorge also spatially orients those undertaking mountain asceticism (shugyo).

 

Mount Myōkō

Mount Myōkō was constructed beginning about 300,000 years ago, in a series of eruptions producing a broad spectrum of lava types including basalt, andesite, and dacite. Its maximum height is estimated to have been between 2,800 metres (9,200 ft) and 2,900 metres (9,500 ft), but it presently reaches only 2,454 metres (8,051 ft). Around 19,000 years ago, the top was blown off in a major eruption, forming a 3 km (2 mi) wide caldera. About 6,000 years ago, the central crater developed and assumed its present shape. A lava dome forms the volcano's present summit. The most recent eruptions about 4,300 years ago produced pyoclastic flows down the eastern flanks. Present activity is solfataric from fumaroles near the lava dome, where sulfur was once mined.


 




Courtesy Google Images