Diluvium
In the Geologic time scale used nowadays in Geology the term Diluvium has been replaced by Pleistocene.
Historically, Diluvium was a term in geology for superficial deposits formed by flood-like operations of water, and so contrasted with alluvium or alluvial deposits formed by slow and steady aqueous agencies. The term was formerly given to the boulder clay deposits, supposed to have been caused by the Noachian deluge.
In the late 20th century Russian geologist Alexei Rudoy proposed the term "diluvium" for description of deposits created as a result of catastrophic outbursts of Pleistocene giant glacier-dammed lakes in intermontane basins of the Altai. The largest of these lakes, Chuya and Kuray, had volumes of water in hundreds of cubic kilometers, and their discharge in peak hydrograph flow rate exceeded the maximum rates of the well-known Pleistocene Lake Missoula floods in North America. The term "diluvium" in the meaning of A. N. Rudoy has become accepted, and the process of diluvial morpholithogenesis can be found in modern textbooks.
Podcasts:
Diluvium
ALBUMS
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Our Sadness
by: DiluviumIt`s growing I hear
In the valley of tears
To send me where I belong
To see my distressful heart.
Is there any sense
There is no more reality
Just throw my self
Floating in the wind.
In this presence of night
It must be seed of new life
Am I still deep inside.
Listen to this cry
For the lost dawn
And unseen setting of sun
We will cry with it
unaware of our sadness.
I`ll never come back
To wish you the same
I took your happiness