 |
1. Primeval Valley of the River Gauja
Sandstone outcrops are found also in most of its tributaries, the valleys and ravines of which merge with the primeval valley of Gauja.
Pay attention!
Next to the cable car, there are stairs leading down the valley, where one can see the slope forest habitats with deadwood, decayed trees, and mushrooms causing a decaying effect to timber. Moss on trees — squirrel-tail moss.
|
 |
2. Krimulda Manor
Both towards the manor house (from the other side and the cable car) and from the manor house, there is a beautiful view over the primeval valley of the River Gauja.
Pay attention!
The romantic landscape park with many old trees, including oaks, established by the first Johan Lieven has survived till nowadays. Suitable place to study moss and lichen (ramalinas, usneas, etc.)
|
 |
3. Piķenes Cliff
Approximately 1 km long and 78-80 m high section of the right side of primeval valley wall of the River Gauja. Along the upper part of Piķenes Cliff, there are forest paths, while along the upper and middle part — Sigulda hiking route. Some places, especially when the trees are without leaves, offer slight outlooks on the primeval valley of the River Gauja.
Pay attention!
Piķenes Cliff is covered in forests of slopes, which are protected habitats. Pre-dominated by oaks, linden trees, maples, and hazel-trees. Suitable place to watch ferns, flowers, moss, lichen, and mushrooms. In the meadow opposite of “Brūveri”, dug-ups by wild boar can be seen, and one might be lucky and spot roe deer on early mornings. Along the bank of the primeval valley of the River Gauja, there are many large decayed trees (home to larvae, door snails, mushrooms, and insects), deadwood. It is the home of various species of woodpeckers leaving traces (besides the bird sounds and songs that are heard) of their “artworks” on the trunks of trees, sulphur shelves. Many types of moss, including squirrel-tail moss.
|
 |
4. Velnala Cliffs
One of the most impressive cliff walls of the valley — around 15 m high; located on the curve of the right bank. From the opposite bank of the River Gauja the dark mouth of Velnala Cave of Krimulda can be seen in the middle of the cliffs. Above Velnala Cave, there are old and biologically valuable pines with the so-called crocodile skin bark. Wooden plank-ways restored on the upper part of cliffs.
|
 |
5. Velnala Cave of Krimulda
The 22.5 m deep (length of galleries — 35 m) cave is formed in the yellow sandstone from Gauja suite 8 m above the water table of Gauja. It is estimated to be around 10,000 years old and created by a spring, which later disappeared and the cave partially fell in. Since 1980, visits to the cave are terminated. Until then, the cave was a popular tourism site. Ancient pagan place. |
 |
6. Pedestrian bridge over the River Gauja
The suspended bridge was constructed in 1976 to make a circular route between Sigulda and Krimulda. Ideal for watching salmons during autumn, when the water is clear.
|
 |
7. Mazā Velna Cave
Heading from Velnala Cliffs in direction of Krimulda along Piķenes Cliff, one cannot pass by without noticing the Mazā Velna Cave, located at the feet of the cliff, opposite of Gauja oxbow lake. The entrance of the cave is split by a sandstone pillar in two parts. Length — 16.5 m, width — 4 m, height — around 2 m.
|
 |
8. Oxbow lakes
Two larger oxbow lakes are seen in the lower part of Piķenes Cliff. Oxbow lakes are the former riverbeds. Where the current has made shortcuts, the old riverbeds no longer expect regular flow of water. Usually the exchange of water takes place during the spring floods, bringing fresh water. Due to the specific hydrologic conditions, special communities of flora and fauna have developed in the oxbow lakes, which is why these are often in the status of protected habitats. Oxbow lakes are often “controlled” by beavers leaving their traces in the oxbow lakes and on the banks thereof. Piķene Beaver Trail has been established here.
|