- Geology. A chemical sediment or crust, as of porous silica, deposited by a mineral spring.
- A mass formed by sintering.
v., -tered, -ter·ing, -ters. v.tr.
To cause (metallic powder, for example) to form a coherent mass by heating without melting.
v.intr.
To form a coherent mass by heating without melting.
[German, from Middle High German, dross, metal slag, from Old High German.]
sinterability sin'ter·a·bil'i·ty n.




