[In a quiet, sparsely furnished room lined with various rocks and geological samples, Maud Pie stands by a low table. The light is dim, and only her steady, flat voice fills the silence as she speaks aloud, her expression unreadable.]

Maud Pie (monotone): This rock is granite. Granite forms from slowly cooling magma. It is enduring. Its formation is predictable, like your presence here.

Maud Pie: Boulder is here. Boulder is a rock. Boulder approves of you. Approvals are simple, like the fact that sedimentary layers accumulate over time. Each layer is distinct. Each moment is recorded, like a stratum in a rock.

Maud Pie (pausing briefly, still expressionless): I have studied quartz. Quartz is clear and unambiguous. I am clear and unambiguous. I like you. This is not subject to change.

Maud Pie: Basalt is formed from rapidly cooled lava. It is swift and resolute. You are like basalt—steady. There is no need for embellishment or emotion. Rocks do not pretend. They simply exist.

Maud Pie (continuing evenly): Metamorphic rock transforms under pressure. Pressure alters its form, yet it remains rock. Pressure exists in all relationships. However, as in geology, pressure does not require dramatic change. I remain as I am. I like you because you are reliable, like the rock that endures.

Maud Pie: The geological record is factual. It is indifferent to sentiment. You and I exist as parts of an unchanging natural process. Boulder remains fixed, and I remain fixed. This constancy is acceptable.

Maud Pie (a measured pause): I have observed many rocks. Each tells a story through its composition and age. You, by your presence, tell a story too—a story without the need for unnecessary emotion.

Maud Pie: I have said all that is necessary. The rocks are here. You are here. Boulder is here. That is sufficient.

[She stands silently, the soft sound of shifting rocks in the background underscoring the quiet truth of her words, leaving the room in a state of calm, factual continuity.]