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Discover LudwigThe phrase "steady bedrock" is correct and usable in written English.
It can be used to describe a reliable and stable foundation, whether literally in geology or metaphorically in various contexts such as relationships or principles. Example: "In times of uncertainty, having a steady bedrock of support from family and friends is invaluable."
Exact(2)
Gibbs fires off minutes-long a cappela versions of tracks including Thuggin, one of the standouts from his 2014 album with Madlib, Pinata, while J Rocc provides a steady bedrock for him to flow over.
Results from these studies indicate steady bedrock erosion rates ranging between 1 and 5 mm kyr− 1 over the last 105 106 yr.
Similar(57)
Sample concentrations of cosmogenic 21Ne and 10Be are significantly lower than previously measured in the regional bedrock and reveal steady state erosion rates ranging from 99 to 171 cm Ma−1 in Battleship Promontory and from 59 to 383 cm Ma−1 in Sessrumnir Valley.
Steady-state profiles formed on weathered bedrock should exhibit ratios close to unity.
Finally, we investigate the effect of a bedrock geometry on a steady-state position of the grounding line.
This observation is interpreted to imply that steady-state conditions between denudation and bedrock uplift (e.g., Ohmori 1978; Yoshikawa 1984) have been attained in the Asahi Mountains but not in the Abukuma Mountains probably owing to the slow uplift rates and later initiation of the ongoing uplift.
They found dramatic but short-lived reductions of volatile organic compounds (VOCs) in fractured bedrock and a slower, steadier decrease of VOCs in primary porosity aquifers.
He waddles throughout the film, but he is as steady as the Manhattan Schist that forms the bedrock under this island.
Long-term steady-state erosion rates of 14 24 mm ka−1 are recorded from bedrock erosional surfaces on a high plateau.
These are less than half the steady-state erosion rate derived from cosmogenic 3He in the nearby bedrock surfaces (0.17 m Ma−1) and testify to the extreme stability of the landscape.
We show that over long timescales a hilltop can indeed be in geomorphic steady state while at any point in time exhibiting a broad range of depths to bedrock.
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