The first barefoot trail created in the Baltic States in the recreation complex "Valguma pasaule", which is located on the forested shores of Lake Valguma. When walking on the path, the feet "massage" sand, wood chips, clay, peat, gravel, cones and various other materials.

Ja Rušona ezeru iepazīstiet ar laivu, tad var apmeklēt Lielo salu (ezera rietumdaļā),kur (augstākajā vietā) ir jāuzmeklē ap 1,2 m augstais akmens. Konstatēts, ka tā apkārtnē un uz virsmas kurināta uguns. Atrastas arī senlietas. Nostāsti vēsta, ka akmens virsmā bijušas iekaltas zīmes (nav saskatāmas) un pie tā upurēti jēri. Tikai nedodieties ezerā, ja ir vai gaidāms stiprs vējš! Rušona ezera salas ir dabas liegums.

One of the highest dunes in Latvia, located between Bernāti and Jūrmalciems villages. It is 37m high and offers a magnificent view of the sea and natural pine forests. The highest dunes in Latvia stand to the South of Jūrmalciems village: the Pūsēnu hill, the Ķupu hill, the Mietragkalns or Tiesas hill, the Pāļu hill, the Garais hill, the Ātrais hill, the Lāvas hill. The Pūsēnu dune is the highest of these dunes which are all called hills by the local people. The Pūsēnu hill developed between 1785 to 1835 when shifting sand became extremely dangerous. Several homesteads were buried in sand, among them „Pūsēni”, where a forester’s family lived. The family is said to have moved to Bārta. The dune was named after the buried homestead.

Jēkabs Janševskis, a Latvian writer, wrote in his book „Nīca”: “In olden times, large pine trees were growing in the dunes on the coast of Nīca and they stood steady and firm. But i Swedish times (around 1650), the Swedes built a large kiln for charcoal and tar. Pine wood and stumps provided an excellent material for this. Once a big fire rose, and the charcoal kiln burned down as well as the whole pine forest. The remaining stumps and bare trunks in the vast burnout could not hold the storm-driven sand; it flew further and further burying not only the burned-out forest, but also the nearest fields. In wintertime, when the vast, low marshy grasslands were covered with ice, jets of sand drifted further over its surface, and soon most of the grasslands and large meadows turned into sandy heath-land and dunes.”

To reconstruct Liepāja, severely damaged during WWII, a silicate brick factory was built in the town. The main raw material was white sand and it was taken from the Bernātu forest. In the 1960-ies they started to dig off the Green Dune and the White Dune, later also the Pūsēnu hill. The excavators used to work day and night, in three shifts. The work stopped at around 1980, as there was no more sand suitable for production of brick.

A trail is set up to facilitate walking in the Pūsēnu Dune in the Bernātu Nature Park.

Sāmsalas ziemeļrietumu daļā jūrā iestiepjas iespaidīgā Tagameizas pussala (Tagamõisa poolsaar). Tās ziemeļrietumu daļā meklējama mazāka – ap 5 km garā Harilaidas pussala (Harilaid). Pussalas vidusdaļā viļņojas Lajalepas ezers (Laialepa järv) - bijušais jūras līcis, kas zemes garozai ceļoties, kļuvis par iekšēju ūdenstilpi. Arī pati Harilaida (igauniski „laid” nozīmē „saliņa”) vairāk nekā trīs gadsimtus atpakaļ bijusi sala. Harilaidu iecienījuši ne tikai migrējošie putni, bet arī roņi, kurus piesaista vientuļi līči un akmeņainās sēres. Harilaidu var apmeklēt tikai ar kājām vai ar divriteni, bet spēkrati ir jāatstāj autostāvlaukumā. No tā ~ 1 km attālumā atrodas vieta, kur pēc 17. gs. radies Harilaidas savienojums ar Sāmsalu. Šeit paveras nepierasti klaja un akmeņaina ainava. Pārējā Harilaidas daļa ir apmežota pirms ~ 40 gadiem. Kopumā būs jāveic ~ 10 km garš pārgājiens.

The trail (the length 1.2 km) introduces with the habitats of dunes and century-old pines, partly covered with sand. Biologists estimate that the oldest tree, the “mother of pines”, could be around 200 years old. Coastal pine forests serve as a barrier between the sea and land protecting inland areas from impact of the sea and winds. Felling coastal forests was forbidden by law already back in 1643, during the Duchy of Courland. Still due to economic activities, the seashore forests were often fell and fires occurred there occasionally. As a result, the sand which had for centuries been hold by trees, started drifting at Cape Kolka. In the 1930ies, there were about 142 hectares of sandy areas in the Slītere National Park, and 11.5 hectares of those were drifting sand. To stop drifting, the sand areas were carefully afforested. Afforestation was started before WW I and it was completed in the 1970ies. To plant new trees, first the sand had to be stopped. Just 26km to the south from Kolka there was one of the largest sand dunes in Latvia, 25km in length. Every year it devoured 0.3 hectares of land. The sand was stopped covering it with heather, twigs and branches of pines and junipers. Pine trees were planted between them.

Today in Kolka, the old, low pine trees tell about the once drifting sand. After storms, when the water washes the bluff and tree roots are exposed, one can see that the tree trunks once have been covered with sand more than 1 meter high. The trees on the seacoast usually have crooked trunks and flag-shaped crowns formed under influence of persisting sea winds. Now these forests are designated biotope “Wooded dunes of the coast”.

Stable white dunes (biotope 2120) do not form in Cape Kolka as they are washed by sea waters during spring and autumn storms. Embryonic dunes develop here (code 2120) with plants that usually grow in dunes. These plants have adapted well to poor soils, heat, drought, and the saline sea water.

The Kolkasrags Pine Trail is in Slītere National Park.

Above and below the town of Kuldīga, the Venta River is distinguished by a variety of biotopes – hillside forests, sandstone and dolomite cliffs, meadows, protected plants and animals, and diverse landscapes. There are popular tourism objects in this part of Kurzeme – the Venta dam, the stone bridge of Kuldīga, the Veckuldīga castle hill, etc. An ecological tourism trail runs along the banks of the Venta, and a bicycling trail has been installed on its left bank.