Biardy: Lapidarium and Glacial Erratics

• The lapidarium contains four glacial erratics: three granites and one gneiss.
• A pegmatite vein with grains of varying sizes and large crystals runs through the smallest granite.
• Established in 2019, the rest and learning site for cyclists includes a shelter, bicycle racks, information boards, waste bins, and a paved surface.
• The margin of the Warta glaciation runs through Biardy, where it is reflected in outwash, kame, and moraine hills.

The lapidarium in Biardy offers a hands-on introduction to the stones on display: visitors can learn more about their age and origin, as well as the characteristics of their surfaces. The information boards at the rest and learning site also cover the rocks on display. This lets you connect information about the glacial erratics with the individual stones instead of simply looking at their names.

The collection can also be divided into rock groups. Three of the glacial erratics are granites, which are intrusive igneous rocks. The fourth is a gneiss and belongs to the metamorphic rocks. This classification gives you a simple starting point for viewing the four exhibits not as a uniform collection, but according to their different classifications.

Looking at their shapes adds to the classification by rock type: the corners, edges, and surfaces of the glacial erratics in Biardy are rounded. This draws attention to the stones' external forms as well as their origins and age. As you explore the collection, you can first look at the four erratics as a group and then take a closer look at individual surface features.

The smallest granite offers a particularly specific detail. A pegmatite vein runs through it, with grains of different sizes and large crystals. Moving between the stone as a whole and this detail makes the collection legible on two levels: as a group of glacial erratics and as an opportunity to examine a single structure more closely.

Information about Biardy's landscape complements the view of the individual stones. The margin of the Warta glaciation runs through the area and is visible in numerous outwash, kame, and moraine hills. These three terms refer to different types of hills, making the landscape description more precise than a general reference to hilly terrain.

This brings two scales together in Biardy: the lapidarium focuses on individual glacial erratics, their surfaces, and their rock groups, while the description of the Warta glaciation turns to landforms. If you are interested in geology, you can understand the area through both specific exhibits and the named hill types.

The rest and learning site was established in 2019. Its amenities include an existing shelter, bicycle racks, waste bins, and a paved surface. Wooden information boards about the rocks on display are also provided. Together, these features create a place to rest and offer information about the stones that are also featured in the lapidarium.

For your travel planning, Biardy offers more than a single point of interest: it brings together a geological exhibit, information about rocks, and a rest and learning site for cyclists. You can weigh up which of these features interests you most by considering the specific topics and details.

Discover more destinations: Łuków, Gołowierzchy, Nowy Świat.

How many glacial erratics are in the lapidarium in Biardy?

The lapidarium contains four glacial erratics: three granites and one gneiss.

What is special about the smallest granite?

A pegmatite vein with grains of varying sizes and large crystals runs through the smallest granite.

What is included at the rest and learning site for cyclists?

It includes a shelter, bicycle racks, wooden information boards about the rocks on display, waste bins, and a paved surface.

To the main travel overview: Łuków.